{"id":21755,"date":"2026-03-17T12:36:20","date_gmt":"2026-03-17T11:36:20","guid":{"rendered":"https:\/\/www.geowiss.uni-mainz.de\/institut-fuer-geowissenschaften\/metamorphe-prozesse\/"},"modified":"2026-07-09T11:56:22","modified_gmt":"2026-07-09T09:56:22","slug":"metamorphic-processes","status":"publish","type":"page","link":"https:\/\/www.geowiss.uni-mainz.de\/en\/institut-fuer-geowissenschaften\/metamorphic-processes\/","title":{"rendered":"Metamorphic Processes"},"content":{"rendered":"\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<jgu-base-anchornavigation react-props=\"{\n    &quot;theme&quot;: &quot;default&quot;,\n    &quot;align&quot;: &quot;wide&quot;\n}\">\n    \n<\/jgu-base-anchornavigation><jgu-base-teaserbox react-props=\"{\n    &quot;headline&quot;: {\n        &quot;htmlTag&quot;: &quot;h2&quot;,\n        &quot;classTag&quot;: &quot;&quot;,\n        &quot;tag&quot;: &quot;h2&quot;\n    },\n    &quot;image&quot;: {\n        &quot;id&quot;: 9714,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/07\\\/Picture1-1.jpg&quot;,\n        &quot;title&quot;: &quot;Picture1&quot;,\n        &quot;width&quot;: 1250,\n        &quot;height&quot;: 700,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/07\\\/Picture1-1.jpg 1250w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/07\\\/Picture1-1-300x168.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/07\\\/Picture1-1-1024x573.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/07\\\/Picture1-1-768x430.jpg 768w&quot;\n    },\n    &quot;color&quot;: &quot;red&quot;,\n    &quot;index&quot;: &quot;Research group&quot;,\n    &quot;title&quot;: &quot;&lt;strong&gt;Metamorphic Processes&lt;\\\/strong&gt;&quot;,\n    &quot;excerpt&quot;: &quot;&lt;strong&gt;Our research focuses on the investigation of rocks exposed to high pressure and temperature conditions during their geodynamic evolution. In particular, we develop thermomechanical models that describe deformation and chemical reactions in rocks and fluids. &lt;\\\/strong&gt;&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;iconColor&quot;: &quot;default&quot;,\n    &quot;isCalendar&quot;: false,\n    &quot;iconBoxed&quot;: false,\n    &quot;useLinkList&quot;: false,\n    &quot;linkList&quot;: {},\n    &quot;hideThumbnail&quot;: false,\n    &quot;type&quot;: &quot;boxed&quot;,\n    &quot;linkTitle&quot;: &quot;&quot;,\n    &quot;linkStyle&quot;: &quot;default&quot;,\n    &quot;overboxImage&quot;: false,\n    &quot;differingHeadlineColor&quot;: false,\n    &quot;headlineColor&quot;: &quot;&quot;,\n    &quot;textPositionBottom&quot;: false,\n    &quot;template&quot;: &quot;&quot;,\n    &quot;video&quot;: {\n        &quot;provider&quot;: &quot;youtube&quot;,\n        &quot;id&quot;: &quot;&quot;,\n        &quot;poster&quot;: &quot;&quot;\n    },\n    &quot;audioUrl&quot;: &quot;&quot;,\n    &quot;unbound&quot;: false\n}\">\n    \n<\/jgu-base-teaserbox><jgu-base-heading react-props=\"{\n    &quot;index&quot;: &quot;AG&quot;,\n    &quot;tags&quot;: {\n        &quot;htmlTag&quot;: &quot;h2&quot;,\n        &quot;classTag&quot;: &quot;&quot;,\n        &quot;tag&quot;: &quot;h2&quot;\n    },\n    &quot;heading&quot;: &quot;Metamorphic Processes&quot;,\n    &quot;textAlign&quot;: &quot;left&quot;,\n    &quot;anchor&quot;: &quot;&quot;,\n    &quot;color&quot;: &quot;red&quot;\n}\"><\/jgu-base-heading>\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">Understanding the Earth requires the integration of various scientific disciplines. Our research focuses on investigating processes in which rocks are exposed to high pressure and temperature conditions during their geodynamic evolution. For this reason, modeling the mechanical behavior of rocks, metamorphic phase equilibria, and physicochemical processes involving fluid interaction that occur within the Earth&#8217;s interior is essential. In our research, we pursue this multidisciplinary approach by using numerical methods, field observations, and geochemical-geochronological data.   <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><jgu-base-image react-props=\"{\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Fluid.gif&quot;,\n        &quot;id&quot;: 14897,\n        &quot;title&quot;: &quot;Fluid&quot;,\n        &quot;width&quot;: 1400,\n        &quot;height&quot;: 1050\n    },\n    &quot;align&quot;: &quot;&quot;,\n    &quot;hasLightbox&quot;: false,\n    &quot;caption&quot;: &quot;&quot;,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-\">\n    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react-props=\"{&quot;selected&quot;:5,&quot;align&quot;:&quot;wide&quot;,&quot;hasAllOpenButton&quot;:true,&quot;onlyOne&quot;:false,&quot;initAllClosed&quot;:true,&quot;enableSearch&quot;:false}\">\n    \n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;Modelling of CHROMium Enrichment in the mantle and the crust (CHROME)&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the DFG, 2024-2027&lt;br\\\/&gt;In collaboration with Prof. Dr. Boris Kaus (Uni. Mainz), Prof. Dr. R. Botcharnikov (Uni. Mainz), Dr. N. Riel (Uni. Mainz), Dr. S. Buhre (Uni. Mainz), Prof. Dr. D. Kostopoulos (Uni. Athens) and Prof. Dr. P. Pomonis (Uni. Athens)&quot;,&quot;slug&quot;:&quot;strongmodelling-of-chromium-enrichment-in-the-mantle-and-the-crust-chrome-strong-brfunded-by-the-dfg-2024-2027brin-collaboration-with-prof-dr-boris-kaus-uni-mainz-prof-dr-r-botcharnikov-uni-mainz-dr-n-riel-uni-mainz-dr-s-buhre-uni-mainz-prof-dr-d-kostopoulos-uni-athens-and-prof-dr-p-pomonis-uni-athens&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">The CHROME project aims to create models for understanding the formation of chromite deposits in ophiolites, focusing on the thermodynamic behavior of multiphase flows. It investigates how chromium behaves during the melting and crystallization processes, noting that despite Cr&#8217;s compatibility, its concentration in melts is not sufficient alone to form chromite deposits, suggesting additional enrichment processes are necessary. The project plans to model the dynamics of melt transport and reactive flows, incorporating various possible enrichment mechanisms, to test hypotheses on chromite formation. Experiments on peridotite rocks containing chromium and multiphase, reactive flow modeling are planned to complement each other, offering insights into ore formation processes. This integrated approach aims to refine our understanding of ore formation, taking into account both experimental results and observations from natural deposits.    <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-right is-layout-flex wp-container-core-group-is-layout-2b4002ad wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/4-768x244-1.jpg&quot;,\n        &quot;id&quot;: 15022,\n        &quot;title&quot;: &quot;4-768x244&quot;,\n        &quot;width&quot;: 768,\n        &quot;height&quot;: 244,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/4-768x244-1.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/4-768x244-1-300x95.jpg 300w&quot;\n    },\n    &quot;caption&quot;: &quot;E&lt;em&gt;&lt;em&gt;Experimental result from natural peridotites (Back-Scattered-Electron Image). (a) The bright areas correspond to interconnected channels of Cr-rich silicate melt on its way to the diamond melt trap (at the top side of the sample). (b) and (c) Elemental maps for Si and Cr, respectively, taken in the area outlined by yellow dashed line in (a).    &lt;\\\/em&gt;&lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;Viscous EffeCTs On Raman-based elasto-thermobarometry (VECTOR): a field, mechanical and diffusion study of mineral inclusions entrapped under a wide range of metamorphic conditions&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the DFG and the National Science Centre (PL), 2024-2026&lt;br\\\/&gt;In collaboration with Prof. Dr. J. Szczepa\\u0144ski (Uni. Wroclaw) and Prof. Dr. M. D\\u0105browski (Polish Geol. Inst.)&quot;,&quot;slug&quot;:&quot;strongviscous-effects-on-raman-based-elasto-thermobarometry-vector-a-field-mechanical-and-diffusion-study-of-mineral-inclusions-entrapped-under-a-wide-range-of-metamorphic-conditions-strong-brfunded-by-the-the-dfg-and-the-national-science-centre-pl-2024-2026brin-collaboration-with-prof-dr-j-szczepanski-uni-wroclaw-and-prof-dr-m-dabrowski-polish-geol-inst&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">Recent advancements like Raman spectroscopy-based elasto-thermobarometry offer a new way to estimate the re-equilibration conditions in a rock&#8217;s history. However, high-temperature irreversible deformation (viscous creep) has been identified to compromise the integrity of minerals&#8217; elastic properties, affecting their ability to retain residual pressure in inclusions. The project aims to develop a new method to quantify the impact of viscous creep on mineral inclusions&#8217; capacity to hold residual pressure, addressing a gap in systematic studies on this issue. Through integrating field data, analytical measurements, and numerical modeling of re-equilibration processes at the mineral level, this project seeks to quantitatively assess the effects of viscous creep and refine the accuracy of determining metamorphic conditions using Raman thermobarometry.   <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-right is-layout-flex wp-container-core-group-is-layout-2b4002ad wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/5-768x298-1.jpg&quot;,\n        &quot;id&quot;: 15028,\n        &quot;title&quot;: &quot;5-768x298&quot;,\n        &quot;width&quot;: 768,\n        &quot;height&quot;: 298,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/5-768x298-1.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/5-768x298-1-300x116.jpg 300w&quot;\n    },\n    &quot;caption&quot;: &quot;&lt;em&gt;&lt;em&gt;Timescale predictions for the exhumation of host-inclusion systems. The predictions are based on the numerical models of temperature-dependent viscoelastic relaxation (see Zhong, &lt;strong&gt;Moulas&lt;\\\/strong&gt;, Taj\\u010dmanov\\u00e1 (2018) for more details). &lt;\\\/em&gt;&lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;A combination of petrological and joint chemical-mechanical inversion approaches to unravel deep geodynamic processes&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the DFG, 2024-2026&lt;br\\\/&gt;In collaboration with Dr. I. Ibragimov (Uni. Mainz)&quot;,&quot;slug&quot;:&quot;stronga-combination-of-petrological-and-joint-chemical-mechanical-inversion-approaches-to-unravel-deep-geodynamic-processes-strong-brfunded-by-the-the-dfg-2024-2026brin-collaboration-with-dr-i-ibragimov-uni-mainz&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">Metamorphism involves the recrystallization of rocks under high temperatures, subjecting them to various pressure and temperature conditions that lead to chemical and mechanical changes in their structure. As metamorphic rocks are brought to the surface, they often retain &#8220;frozen&#8221; evidence of these processes due to the rapid cooling they undergo, preserving high-temperature traces like chemically zoned crystals and stresses within mineral inclusions. Recent advancements in diffusion modeling and Raman elastic barometry have enhanced our understanding of these changes in natural rocks. This study aims to develop inverse models that could jointly infer the mechanical and chemical relaxation of metamorphic textures. Such models can be corroborated using geodynamic models that predict the P-T evolution of rocks. Focusing on metamorphic rocks, the approach seeks to quantify the slow, often imperceptible metamorphic processes that occur under the Earth&#8217;s surface (see for example publication numbers <em>Ibragimov, Kiss, <strong>Moulas<\/strong>, (2024)<\/em> and <em>Schorn, <strong>Moulas<\/strong>, St\u00fcwe (2024)<\/em> for more details).     <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-right is-layout-flex wp-container-core-group-is-layout-2b4002ad wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/UntitledProject3-ezgif.com-crop-2.gif&quot;,\n        &quot;id&quot;: 15032,\n        &quot;title&quot;: &quot;UntitledProject3-ezgif.com-crop-2&quot;,\n        &quot;width&quot;: 599,\n        &quot;height&quot;: 220\n    },\n    &quot;caption&quot;: &quot;&lt;em&gt;&lt;em&gt;&lt;em&gt;Geodynamic simulation of lithospheric convergence and continental subduction. The different rock units move through space and experience a variety of conditions. Thermally-activated processes such as solid-state mineral diffusion and viscous relaxation (creep) will occur in the deforming metamorphic rocks depending on the different paths taken by the rocks. The forward simulation of such processes will lead to a better understanding of the integrated geological data.   &lt;\\\/em&gt;&lt;\\\/em&gt;&lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;Uncertain Nonlinearities in Groundwater Flow Models&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the M3ODEL Institute and RWTH Aachen, 2020-2025&lt;br\\\/&gt;In collaboration with Prof. Dr. M. Bachmayr (Applied Mathematics \\u2013 RWTH Aachen)&lt;br&gt;  &quot;,&quot;slug&quot;:&quot;stronguncertain-nonlinearities-in-groundwater-flow-models-strong-brfunded-by-the-m3odel-institute-and-rwth-aachen-2020-2025brin-collaboration-with-prof-dr-m-bachmayr-applied-mathematics-rwth-aachenbr&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">The fluid flow in porous rocks is governed by complex and non-linear Partial Differential Equations (PDEs). In this project we are investigating the solvability and the behavior of non-linear porous-flow equations. These equations describe the fluid flow within deforming rocks. In particular, the complex volumetric rheology of rocks is investigated. The results of this study have many implications for energy applications that include the integrity and the permeability evolution of reservoir rocks.    <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-center is-layout-flex wp-container-core-group-is-layout-524f8de7 wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/geoTest2bSmooth_animation.gif&quot;,\n        &quot;id&quot;: 14893,\n        &quot;title&quot;: &quot;geoTest2bSmooth_animation&quot;,\n        &quot;width&quot;: 1600,\n        &quot;height&quot;: 1200\n    },\n    &quot;caption&quot;: &quot;&lt;em&gt;Porosity evolution (top row) and effective pressure evolution (bottom row) during compaction-driven fluid flow. The computational grid on the right spans the whole space-time domain. Figure courtesy of S. Boisser\\u00e9e.  &lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;Grain-scale pressure variations in metamorphic rocks&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the M3ODEL Institute and the Alexander von Humboldt Foundation, 2020-2024&lt;br\\\/&gt;In collaboration with Dr. M. Mazzucchelli (Uni. Lausanne), &amp; Prof. Y. Podladchikov (Uni. Lausanne)&lt;br&gt;&quot;,&quot;slug&quot;:&quot;stronggrain-scale-pressure-variations-in-metamorphic-rocks-strong-brfunded-by-the-m3odel-institute-and-the-alexander-von-humboldt-foundation-2020-2024brin-collaboration-with-dr-m-mazzucchelli-uni-lausanne-prof-y-podladchikov-uni-lausannebr&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">Metamorphic rocks are always deformed when recrystallized. Even in the absence of far-field deformation, the volumetric thermoelastic strains can lead to the development of GPa-level stresses at the mineral scale. For this reason, we develop new mechanical models that allow the quantification of the deformation in composite materials such as rocks. Such models are tested using spectroscopic techniques (e.g. Raman Spectroscopy) and can provide insightful information regarding the development of residual stresses.   <\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-center is-layout-flex wp-container-core-group-is-layout-524f8de7 wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/2-768x393-1.jpg&quot;,\n        &quot;id&quot;: 15008,\n        &quot;title&quot;: &quot;2-768x393&quot;,\n        &quot;width&quot;: 768,\n        &quot;height&quot;: 393,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/2-768x393-1.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/2-768x393-1-300x154.jpg 300w&quot;\n    },\n    &quot;caption&quot;: &quot;&lt;em&gt;&lt;em&gt;A: Schematic representation of the elasto-plastic zone that develops at a host-inclusion interface. B: stress distribution around a pressurized mineral inclusion (see &lt;strong&gt;Moulas&lt;\\\/strong&gt; et al (2020), Pl\\u00fcmper, Wallis, Teuling, &lt;strong&gt;Moulas&lt;\\\/strong&gt;  &lt;\\\/em&gt;&lt;\\\/em&gt;&lt;em&gt;et al. (2022) and &lt;strong&gt;Moulas&lt;\\\/strong&gt; et al (2023)&lt;em&gt; for more details).&lt;\\\/em&gt; &lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<jgu-base-accordionitem react-props=\"{&quot;title&quot;:&quot;&lt;strong&gt;Thermodynamic equilibrium and stress evolution of metamorphic rocks&lt;\\\/strong&gt;&lt;br\\\/&gt;Funded by the M3ODEL institute, the Alexander von Humboldt foundation (2020-2023) and the University of Lausanne (2024-..)&lt;br\\\/&gt;In collaboration with Dr. M. Mazzucchelli (Uni. Lausanne), Prof. Dr. S. Schmalholz (Uni. Lausanne) &amp; Prof. Dr. T. Speck (Uni. Stuttgart)&quot;,&quot;slug&quot;:&quot;strongthermodynamic-equilibrium-and-stress-evolution-of-metamorphic-rocks-strong-brfunded-by-the-m3odel-institute-the-alexander-von-humboldt-foundation-2020-2023-and-the-university-of-lausanne-2024-brin-collaboration-with-dr-m-mazzucchelli-uni-lausanne-prof-dr-s-schmalholz-uni-lausanne-prof-dr-t-speck-uni-stuttgart&quot;,&quot;align&quot;:&quot;wide&quot;,&quot;init&quot;:true,&quot;customSlug&quot;:false}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-big-font-size wp-block-paragraph\">The development of stresses in minerals affects their energy. As a result, the stability of metamorphic mineral assemblages does not depend on a simple &#8220;pressure&#8221; value and more complex theories are needed. In this research direction, we investigate the thermodynamic equilibrium of stressed rocks by means of:  <\/p>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\">i) deformation experiments corroborated by thermomechanical simulations<\/p>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\">ii) hydro-chemo-mechanical modeling (multiphase flow equations)<\/p>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\">iii) classical molecular dynamics simulations<\/p>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\">Our results can be used to create predictive models that can account for the effects of deformation on mineral reactions (see <em>Cionoiu, <strong>Moulas<\/strong>, Taj\u010dmanov\u00e1 (2019)<\/em>, <em>Schmalholz, <strong>Moulas<\/strong> et al. (2020), Cionoiu, <strong>Moulas<\/strong>, St\u00fcnitz, Taj\u010dmanov\u00e1 (2022) <\/em>, <em>Schmalholz,<strong> Moulas,<\/strong> R\u00e4ss, M\u00fcntener<\/em>, <em>(2023)<\/em> and <em>Mazzucchelli, <strong>Moulas,<\/strong> Kaus, Speck, (2024)<\/em> for more details).<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-group is-vertical is-content-justification-right is-layout-flex wp-container-core-group-is-layout-2b4002ad wp-block-group-is-layout-flex\" style=\"box-shadow:var(--wp--preset--shadow--natural)\">\n<div style=\"height:55px\" aria-hidden=\"true\" class=\"wp-block-spacer wp-container-content-0591978f\"><\/div>\n\n\n<jgu-base-image react-props=\"{\n    &quot;align&quot;: &quot;right&quot;,\n    &quot;image&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/3.gif&quot;,\n        &quot;id&quot;: 15020,\n        &quot;title&quot;: &quot;3&quot;,\n        &quot;width&quot;: 800,\n        &quot;height&quot;: 200\n    },\n    &quot;caption&quot;: &quot;&lt;em&gt;Example of a molecular dynamics simulation of the coexistence of a stressed solid with a melt of the same composition (see publication [38] for more details)&lt;\\\/em&gt;&quot;,\n    &quot;width&quot;: 0,\n    &quot;hasLightbox&quot;: false,\n    &quot;imgWidth&quot;: 0,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-right\">\n    \n<\/jgu-base-image>\n\n\n<div style=\"height:9px\" aria-hidden=\"true\" class=\"wp-block-spacer wp-container-content-579443fb\"><\/div>\n<\/div>\n<\/div>\n<\/div>\n\n\n<\/jgu-base-accordionitem>\n\n<\/jgu-base-accordion>\n\n\n\n<div class=\"wp-block-group alignwide is-layout-constrained wp-block-group-is-layout-constrained\"><jgu-base-heading 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Simon&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 25036,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Simon.jpg&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Simon&quot;,\n        &quot;width&quot;: 400,\n        &quot;height&quot;: 400,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Simon.jpg 400w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Simon-300x300.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Simon-150x150.jpg 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;Academic staff members&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;boisseree &lt;em&gt;at&lt;\\\/em&gt; uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;external-link-alt-solid&quot;,\n    &quot;title&quot;: &quot;&lt;a href=\\&quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/337016\\&quot; target=\\&quot;_blank\\&quot; rel=\\&quot;noreferrer noopener\\&quot;&gt;Profile&lt;\\\/a&gt;&quot;,\n    &quot;uuid&quot;: &quot;1783508167564&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/337016&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard>\n\n\n<div style=\"height:45px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<jgu-base-button style=\"display: flex; flex-wrap: wrap; column-gap: 30px; max-width: 100%; flex-direction: row; justify-content: left\">\n  \n<jgu-base-buttonitem react-props=\"{\n    &quot;text&quot;: &quot;Homepage&quot;,\n    &quot;icon&quot;: &quot;user-check-solid&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot; \\nhttps:\\\/\\\/boisseree.github.io&quot;,\n        &quot;opensInNewTab&quot;: true\n    },\n    &quot;align&quot;: &quot;left&quot;,\n    &quot;styling&quot;: &quot;primary&quot;,\n    &quot;type&quot;: &quot;default&quot;,\n    &quot;iconBefore&quot;: false,\n    &quot;isSmall&quot;: false,\n    &quot;fullWidth&quot;: false,\n    &quot;className&quot;: &quot;&quot;\n}\"><\/jgu-base-buttonitem>\n\n<\/jgu-base-button><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\">\n\n<jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Riel, Dr. Nicolas&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 25057,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Nicolas.jpg&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Nicolas&quot;,\n        &quot;width&quot;: 400,\n        &quot;height&quot;: 400,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Nicolas.jpg 400w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Nicolas-300x300.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Nicolas-150x150.jpg 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;Academic staff members&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;nriel &lt;em&gt;at&lt;\\\/em&gt; uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;external-link-alt-solid&quot;,\n    &quot;title&quot;: &quot;&lt;a href=\\&quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/12469\\&quot; target=\\&quot;_blank\\&quot; rel=\\&quot;noreferrer noopener\\&quot;&gt;Profile&lt;\\\/a&gt;&quot;,\n    &quot;uuid&quot;: &quot;1783508167564&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/12469&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\">\n\n<jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Stroh, Annalena&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 25074,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Annalena.jpg&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Annalena&quot;,\n        &quot;width&quot;: 400,\n        &quot;height&quot;: 400,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Annalena.jpg 400w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Annalena-300x300.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/07\\\/Annalena-150x150.jpg 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;PhD Students&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;anstroh &lt;em&gt;at&lt;\\\/em&gt; uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;external-link-alt-solid&quot;,\n    &quot;title&quot;: &quot;&lt;a href=\\&quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/9111\\&quot; target=\\&quot;_blank\\&quot; rel=\\&quot;noreferrer noopener\\&quot;&gt;Profile&lt;\\\/a&gt;&quot;,\n    &quot;uuid&quot;: &quot;1783508167564&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/personen.uni-mainz.de\\\/person\\\/9111&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><\/div>\n<\/div>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><strong>MSc and BSc students<\/strong><\/p>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Fe\\u00dfler, Claudia&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 15569,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ol_XPL_y192102022009.webp&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Ol_XPL_y192102022009&quot;,\n        &quot;width&quot;: 722,\n        &quot;height&quot;: 722,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ol_XPL_y192102022009.webp 722w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ol_XPL_y192102022009-300x300.webp 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ol_XPL_y192102022009-150x150.webp 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;MSc student&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;cfessler &lt;em&gt;at&lt;\\\/em&gt; students.uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Lamest, Stella&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 15142,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Z1_210212201202.webp&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Z1_210212201202&quot;,\n        &quot;width&quot;: 1280,\n        &quot;height&quot;: 720,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Z1_210212201202.webp 1280w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Z1_210212201202-300x169.webp 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Z1_210212201202-1024x576.webp 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Z1_210212201202-768x432.webp 768w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;MSc student&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;slamest &lt;em&gt;at&lt;\\\/em&gt; students.uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Vakhitova, Katerina&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 15574,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Fa-Ap_PPL_Y10_210219194829.webp&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Fa-Ap_PPL_Y10_210219194829&quot;,\n        &quot;width&quot;: 722,\n        &quot;height&quot;: 723,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Fa-Ap_PPL_Y10_210219194829.webp 722w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Fa-Ap_PPL_Y10_210219194829-300x300.webp 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Fa-Ap_PPL_Y10_210219194829-150x150.webp 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;MSc student&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;kvakhito &lt;em&gt;at&lt;\\\/em&gt; students.uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n\n\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;Lotz, Katharina&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: 15583,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ms-Gt_XPL_G100210129210019.webp&quot;,\n        &quot;credit&quot;: &quot;&quot;,\n        &quot;title&quot;: &quot;Ms-Gt_XPL_G100210129210019&quot;,\n        &quot;width&quot;: 722,\n        &quot;height&quot;: 722,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ms-Gt_XPL_G100210129210019.webp 722w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ms-Gt_XPL_G100210129210019-300x300.webp 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Ms-Gt_XPL_G100210129210019-150x150.webp 150w&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;actions&quot;: [],\n    &quot;color&quot;: &quot;default&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;address-card-solid&quot;,\n    &quot;title&quot;: &quot;BSc student&quot;,\n    &quot;uuid&quot;: &quot;1773144921640&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;icon&quot;: &quot;envelope-solid&quot;,\n    &quot;title&quot;: &quot;klotz01 &lt;em&gt;at&lt;\\\/em&gt; students.uni-mainz.de&lt;br&gt;&quot;,\n    &quot;uuid&quot;: &quot;1773145031183&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;\n    }\n}\">\n    \n<\/jgu-base-listitem>\n\n<\/jgu-base-contactcard><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\"><\/div>\n<\/div>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><strong>Former group members<\/strong><\/p>\n\n\n<ul class=\"styled-list hyphenation\">\n\t\n<ul class=\"styled-list hyphenation\"><jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;&lt;strong&gt;Doctoral candidates &amp; academic staff members&lt;\\\/strong&gt;&quot;,\n    &quot;uuid&quot;: &quot;1783587086848&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: null\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;&lt;br&gt;Dr. Iskander Ibragimov (Utrecht University)&quot;,\n    &quot;uuid&quot;: &quot;1783587152405&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: null\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;Dr. Mattia Mazzucchelli (University of Lausanne)&quot;,\n    &quot;uuid&quot;: &quot;1783587152405&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: null\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;Dr. Dimitrios Moutzouris (Goethe University Frankfurt)&quot;,\n    &quot;uuid&quot;: &quot;1783587564908&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;,\n    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true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;&lt;br&gt;Diana Daubner (Baugrundinstitut Franke-Mei\\u00dfner und Partner GmbH) &quot;,\n    &quot;uuid&quot;: &quot;1783587152405&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: null\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    &quot;allowNesting&quot;: true,\n    &quot;icon&quot;: &quot;&quot;,\n    &quot;showExpandableContent&quot;: false,\n    &quot;expandableContent&quot;: &quot;&quot;\n}\">\n    \n<\/jgu-base-listitem>\n\n<jgu-base-listitem react-props=\"{\n    &quot;title&quot;: &quot;Jana David (Baugrundinstitut Franke-Mei\\u00dfner und Partner GmbH) &quot;,\n    &quot;uuid&quot;: &quot;1783587564908&quot;,\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;showInActions&quot;: false,\n    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&quot;caption&quot;: &quot;&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;&quot;,\n        &quot;target&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;\n    }\n}\" class=\"align-center\">\n    \n<\/jgu-base-image>\n\n\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group alignwide is-layout-constrained wp-block-group-is-layout-constrained\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><jgu-base-tabs react-props=\"{\n    &quot;metadata&quot;: {\n        &quot;name&quot;: &quot;Lehrveranstaltungen&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;selected&quot;: 1,\n    &quot;ratio&quot;: 0,\n    &quot;autoRatio&quot;: true,\n    &quot;stackMobile&quot;: false,\n    &quot;hasAllOpenButton&quot;: true,\n    &quot;onlyOne&quot;: false,\n    &quot;initAllClosed&quot;: true,\n    &quot;enableSearch&quot;: false,\n    &quot;layout&quot;: {\n        &quot;type&quot;: &quot;flex&quot;,\n        &quot;flexWrap&quot;: &quot;nowrap&quot;,\n        &quot;justifyContent&quot;: &quot;space-between&quot;,\n        &quot;orientation&quot;: &quot;horizontal&quot;\n    }\n}\">\n    \n<jgu-base-tabsitem react-props=\"{\n    &quot;title&quot;: &quot;BSc courses&quot;,\n    &quot;slug&quot;: &quot;bsc-veranstaltungen&quot;,\n    &quot;metadata&quot;: {\n        &quot;name&quot;: &quot;BSc Geowissenschaften&quot;\n    },\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;customSlug&quot;: false\n}\">\n    \n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-8f761849 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Compulsory Module Endogenous Geology<\/strong> &#8211; M.09.065.010.B<\/p>\n\n\n\n<ul class=\"wp-block-list has-small-font-size\">\n<li><strong>Fundamentals of Endogenous Geology &#8211; 09.065.011.B<\/strong> | C. Helo<\/li>\n\n\n\n<li><strong>Petrological internship (endogenous) &#8211; 09.065.012.B<\/strong> | C.Helo<\/li>\n\n\n\n<li><strong>Field Internship (endogenous) &#8211; 09.065.013.B<\/strong> | C. Helo, K. Seelos <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Compulsory Module Petrology<\/strong> &#8211; M.09.065.062.B (together with Petrology working group)<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Petrology of magmatic and metamorphic rocks &#8211; 09.065.062.B  <\/strong> | R. Botcharnikov, E. Moulas<\/li>\n\n\n\n<li><strong>Petrology of magmatic and metamorphic rocks practice class <\/strong>  &#8211; <strong>09.065.063.B<\/strong> | R. Botcharnikov, S. Buhre, E. Moulas <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Compulsory Module Geological Fieldwork<\/strong> &#8211; M.09.065.050.B <\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Day Excursion 1 &#8211; 09.065.053.B<\/strong> | S. Buhre, C. Helo<\/li>\n\n\n\n<li><strong>Day Excursion 2 &#8211; 09.065.054.B<\/strong> | R. Botcharnikov, E. Moulas<\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Elective Module Dynamic Processes and Data Science<\/strong> &#8211; M.09.065.220.B <\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Dynamic Processes and Data Science &#8211; 09.065.221.B<\/strong> | R. Botcharnikov, B. Kaus, E. Moulas <\/li>\n\n\n\n<li><strong>Dynamic Processes and Data Science &#8211; 09.065.222.B<\/strong> | B. Kaus, E. Moulas <\/li>\n\n\n\n<li> <strong>Big Data and Machine Learning<\/strong> &#8211; <strong>09.065.223.B<\/strong> | E. Moulas <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Extracurricular Events<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Anatomy of rock-forming minerals<\/strong> | C. Helo<\/li>\n\n\n\n<li><strong>BSc\/MSc Project seminar<\/strong> | C. 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Moulas <\/li>\n\n\n\n<li><strong>Volcanology (thermodynamic aspects) &#8211; 09.065.M522<\/strong> | C. Helo <\/li>\n\n\n\n<li><strong>MSc Petrology Project &#8211; 09.065.M522<\/strong> | R. Botcharnikov, S. Buhre, C. Helo, E. Moulas<\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Elective Module Dynamics of the Lithosphere<\/strong> &#8211; M.09.065.505<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Orogenic Systems &#8211; 09.065.M533<\/strong> | R. Botcharnikov, J. Castro, E. Moulas <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Elective Module Geodynamical and Petrological Methods<\/strong> &#8211; M.09.065.570<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Mineral Equilibria Modelling &#8211; 09.065.M572<\/strong> | E. Moulas <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Compulsory Module Field<\/strong> &#8211; M.09.065.500<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Field Course Exogenous Geology &#8211; 09.065.M503<\/strong> | F. Hawemann, C. Helo<\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-normal-font-size wp-block-paragraph\"><strong>Extracurricular Events<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Anatomy of rock-forming minerals<\/strong> | C. Helo<\/li>\n\n\n\n<li><strong>BSc\/MSc Project seminar<\/strong> | C. 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&quot;&quot;,\n    &quot;index&quot;: &quot;&quot;\n}\"><\/jgu-base-heading>\n\n\n\n<div class=\"wp-block-group is-content-justification-center is-layout-constrained wp-block-group-is-layout-constrained\">\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><strong>2026<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[14]<\/strong> <strong>Moulas E<\/strong> (2026). Numerical Modelling of Geological Processes, with emphasis on Geochemistry, Petrology and Geochronology (Workshop Lecture Notes and Codes). Zenodo. doi: <a href=\"https:\/\/doi.org\/10.5281\/zenodo.18413414\">10.5281\/zenodo.18413414<\/a>.   <\/p>\n<\/div>\n\n\n\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><strong>2025<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[13]<\/strong> <strong>Moulas E<\/strong> (2025) TEMP2D: A simple thermo-kinematic model for rock exhumation in 2-D. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15830073\">10.5281\/zenodo.15830072<\/a>   <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[12]<\/strong> Stroh A, Aellig P, <strong>Moulas E<\/strong> (2025) AnStroh\/MovingBoundaryMinerals.jl: v0.1.0. (A Julia package for the calculation of chemical diffusion in growing crystals). Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15546347\">10.5281\/zenodo.15535732<\/a>    <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[11]<\/strong> Riel N, Kaus B, de Montserrat A, <strong>Moulas E<\/strong>, Green E, Dominguez H (2025) An unconstrained formulation for complex solution phase minimization (Codes). Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/13982544\">10.5281\/zenodo.13982543<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[10]<\/strong> Porkol\u00e1b K, <strong>Moulas E<\/strong>, Schmalholz SM (2025) Code and thermodynamic data for a 2D hydro-mechanical-chemical model of antigorite dehydration. Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/14202518\">10.5281\/zenodo.14202517<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><strong>2024<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[9]<\/strong> Boisser\u00e9e S, <strong>Moulas E<\/strong>, Bachmayr M (2024) Fluid flow channeling and mass transport with discontinuous porosity distribution (Julia code for hydromechanical solver and chemical postprocessing). Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15758079\">10.5281\/zenodo.13986982<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[8]<\/strong> Schorn S, <strong>Moulas E<\/strong> (2024) ZirTiDiS: an implicit finite difference code for the calculation of apparent Zr-in-Titanite (ZiT) temperatures. Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/11184086\">10.5281\/zenodo.11184085<\/a>   <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[7]<\/strong> Stroh A, <strong>Moulas E<\/strong>, Botcharnikov R (2024) FIDDO: FInite Difference Diffusion in Olivine. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/10964860\">10.5281\/zenodo.10964859<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[6]<\/strong> <strong>Moulas E<\/strong>, Schorn S (2024) T1dH: A 1-d code for the calculation of Heat conduction with Earth Science Applications. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/11046566\">10.5281\/zenodo.11046565<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><strong>2023<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[5] Moulas E<\/strong> (2023) Numerical Modelling of Chemical Diffusion in Petrology and Geochemistry (Workshop Lecture Notes). Zenodo. <a href=\"https:\/\/zenodo.org\/records\/10053579\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.10047582<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[4] Moulas E<\/strong> (2023) GDIFF: a Finite Difference code for the calculation of multicomponent diffusion in garnet. Zenodo. <a href=\"https:\/\/zenodo.org\/record\/7940212\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.7805989<\/a>  <\/p>\n<\/div>\n\n\n\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><strong>2022<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[3] Moulas E<\/strong>, Brandon MT (2022) KADMOS: a Finite Element code for the calculation of apparent K-Ar ages in minerals. Zenodo. <a href=\"https:\/\/zenodo.org\/record\/7358138#.ZDBc-tJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.7358138<\/a> <\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[2]<\/strong> Cionoiu S, <strong>Moulas E<\/strong>, Taj\u010dmanov\u00e1 L (2022) Local variation of mechanical parameters in (Griggs-type) viscous deformation experiments (Matlab code). <a href=\"https:\/\/zenodo.org\/record\/6951760#.ZDBdVNJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.6951759<\/a><\/p>\n<\/div>\n\n\n\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-grid wp-container-core-group-is-layout-30d3fc08 wp-block-group-is-layout-grid\">\n<p class=\"has-big-font-size wp-container-content-2c2f8874 wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-big-font-size wp-container-content-adee2e7b wp-block-paragraph\"><strong>[1]<\/strong> <strong>Moulas E<\/strong>, Kaus B, Jamtveit B (2022) Dynamic Pressure Variations in the Lower Crust Caused by Localized Fluid-Induced Weakening (LaMEM input files). <a href=\"https:\/\/zenodo.org\/record\/6538290#.ZDBdttJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi: 10.5281\/zenodo.6538290<\/a><\/p>\n<\/div>\n<\/div>\n\n\n\n<p class=\"has-big-font-size wp-block-paragraph\"><\/p>\n<\/div><\/div>\n<\/jgu-base-section><jgu-base-section react-props=\"{&quot;color&quot;:&quot;dark&quot;,&quot;metadata&quot;:{&quot;name&quot;:&quot;Publikationen&quot;},&quot;align&quot;:&quot;wide&quot;,&quot;padding&quot;:&quot;medium&quot;}\">\n<div class=\"jgu-bgsection bg bg-dark \"><div class=\"content padding-medium\"><div\n\tclass=\"jgu-anchorpoint\"\n\tid=\"publications\"\n\tdata-label=\"Publications\"\n\tdata-hide-in-nav=\"false\"\n\ttabindex=\"0\"\n\tdata-initial-scroll=\"true\"\n><\/div>\n\n\n<jgu-base-heading react-props=\"{\n    &quot;color&quot;: &quot;default&quot;,\n    &quot;tags&quot;: {\n        &quot;htmlTag&quot;: &quot;h2&quot;,\n        &quot;classTag&quot;: &quot;&quot;,\n        &quot;tag&quot;: &quot;h2&quot;\n    },\n    &quot;heading&quot;: &quot;Publications&quot;,\n    &quot;className&quot;: &quot;&quot;,\n    &quot;textAlign&quot;: &quot;left&quot;,\n    &quot;anchor&quot;: &quot;&quot;,\n    &quot;index&quot;: &quot;&quot;\n}\"><\/jgu-base-heading>\n\n\n\n\n<jgu-base-fis react-props=\"{\n    &quot;user&quot;: &quot;evmoulas&quot;,\n    &quot;endPoint&quot;: &quot;user&quot;,\n    &quot;equipment&quot;: &quot;&quot;,\n    &quot;tag&quot;: &quot;&quot;,\n    &quot;orgStructure&quot;: &quot;&quot;,\n    &quot;project&quot;: &quot;&quot;,\n    &quot;n&quot;: &quot;&quot;,\n    &quot;style&quot;: &quot;apa-jgu&quot;,\n    &quot;type&quot;: &quot;&quot;,\n    &quot;year&quot;: &quot;&quot;,\n    &quot;openAll&quot;: true\n}\">\n    \n<\/jgu-base-fis><\/div><\/div>\n<\/jgu-base-section>    <div style=\"display: none\">\n        \n    <\/div>","protected":false},"excerpt":{"rendered":"<p>Understanding the Earth requires the integration of various scientific disciplines. Our research focuses on investigating processes in which rocks are exposed to high pressure and temperature conditions during their geodynamic evolution. For this reason, modeling the mechanical behavior of rocks, metamorphic phase equilibria, and physicochemical processes involving fluid interaction that occur within the Earth&#8217;s interior &hellip; <a href=\"https:\/\/www.geowiss.uni-mainz.de\/en\/institut-fuer-geowissenschaften\/metamorphic-processes\/\">Continued<\/a><\/p>\n","protected":false},"author":1931,"featured_media":0,"parent":21238,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"categories":[143],"tags":[149],"class_list":["post-21755","page","type-page","status-publish","hentry","category-work-groups","tag-metamorphic-processes-work-group"],"content_raw":"<!-- wp:spacer {\"height\":\"10px\"} -->\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer --><!-- wp:jgu\/anchornavigation {\"theme\":\"default\"} \/--><!-- wp:jgu\/teaserbox {\"headline\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"image\":{\"id\":9714,\"url\":null},\"color\":\"red\",\"index\":\"Research group\",\"title\":\"\\u003cstrong\\u003eMetamorphic Processes\\u003c\/strong\\u003e\",\"excerpt\":\"\\u003cstrong\\u003eOur research focuses on the investigation of rocks exposed to high pressure and temperature conditions during their geodynamic evolution. In particular, we develop thermomechanical models that describe deformation and chemical reactions in rocks and fluids. \\u003c\/strong\\u003e\"} \/--><!-- wp:jgu\/heading {\"index\":\"AG\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Metamorphic Processes\"} \/--><!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">Understanding the Earth requires the integration of various scientific disciplines. Our research focuses on investigating processes in which rocks are exposed to high pressure and temperature conditions during their geodynamic evolution. For this reason, modeling the mechanical behavior of rocks, metamorphic phase equilibria, and physicochemical processes involving fluid interaction that occur within the Earth's interior is essential. In our research, we pursue this multidisciplinary approach by using numerical methods, field observations, and geochemical-geochronological data.   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14897}} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><!-- wp:jgu\/section {\"color\":\"white-dark-text\",\"metadata\":{\"name\":\"News\"}} -->\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"News\",\"slug\":\"news\",\"className\":\"\"} \/-->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"News\",\"className\":\"\"} \/-->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:jgu\/teaserbox 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number\",\"width\":0} \/--><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"35%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:35%\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15119},\"width\":0} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"h3\",\"tag\":\"h2.h3\"},\"heading\":\"Research Interests\"} \/-->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"60%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:60%\"><!-- wp:jgu\/list -->\n<ul class=\"styled-list hyphenation\"><!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eMetamorphic phase equilibria\\u003c\/strong\\u003e\",\"uuid\":\"1774432193306\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eLocal equilibrium thermodynamics in Earth systems\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eDiffusion and transport phenomena in geomaterials\\u003c\/strong\\u003e\",\"uuid\":\"1774432193306\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eNumerical modeling of rock deformation and fluid flows\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eInteraction between deformation and phase equilibria\\u003c\/strong\\u003e\",\"uuid\":\"1774432193306\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eThermo-mechanical modeling with geological applications\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eNon-stationary temperature and pressure variations in the crust and lithosphere\\u003c\/strong\\u003e\",\"uuid\":\"1774432193306\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003e\\u003cstrong\\u003eFluid flows\\u003c\/strong\\u003e and solitary waves in the Earth's body\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eMetamorphic Geology of high-grade\\u003cem\\u003e \\u003c\/em\\u003eterranes\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eTectonics and geodynamics of mountain belts\\u003c\/strong\\u003e\",\"uuid\":\"1774432193306\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003e\\u003cstrong\\u003eGeodynamic evolution of the Alpine-Himalayan mountain belt\\u003c\/strong\\u003e\\u003c\/strong\\u003e\",\"uuid\":\"1774432220926\",\"link\":{\"url\":null}} \/--><\/ul>\n<!-- \/wp:jgu\/list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:separator -->\n<hr class=\"wp-block-separator has-alpha-channel-opacity\" \/>\n<!-- \/wp:separator -->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"h3\",\"tag\":\"h2.h3\"},\"heading\":\"Ongoing research projects (selection)\"} \/-->\n\n<!-- wp:jgu\/accordion {\"selected\":5} -->\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eModelling of CHROMium Enrichment in the mantle and the crust (CHROME)\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the DFG, 2024-2027\\u003cbr\/\\u003eIn collaboration with Prof. Dr. Boris Kaus (Uni. Mainz), Prof. Dr. R. Botcharnikov (Uni. Mainz), Dr. N. Riel (Uni. Mainz), Dr. S. Buhre (Uni. Mainz), Prof. Dr. D. Kostopoulos (Uni. Athens) and Prof. Dr. P. Pomonis (Uni. Athens)\",\"slug\":\"strongmodelling-of-chromium-enrichment-in-the-mantle-and-the-crust-chrome-strong-brfunded-by-the-dfg-2024-2027brin-collaboration-with-prof-dr-boris-kaus-uni-mainz-prof-dr-r-botcharnikov-uni-mainz-dr-n-riel-uni-mainz-dr-s-buhre-uni-mainz-prof-dr-d-kostopoulos-uni-athens-and-prof-dr-p-pomonis-uni-athens\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The CHROME project aims to create models for understanding the formation of chromite deposits in ophiolites, focusing on the thermodynamic behavior of multiphase flows. It investigates how chromium behaves during the melting and crystallization processes, noting that despite Cr's compatibility, its concentration in melts is not sufficient alone to form chromite deposits, suggesting additional enrichment processes are necessary. The project plans to model the dynamics of melt transport and reactive flows, incorporating various possible enrichment mechanisms, to test hypotheses on chromite formation. Experiments on peridotite rocks containing chromium and multiphase, reactive flow modeling are planned to complement each other, offering insights into ore formation processes. This integrated approach aims to refine our understanding of ore formation, taking into account both experimental results and observations from natural deposits.    <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"right\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15022},\"caption\":\"E\\u003cem\\u003e\\u003cem\\u003eExperimental result from natural peridotites (Back-Scattered-Electron Image). (a) The bright areas correspond to interconnected channels of Cr-rich silicate melt on its way to the diamond melt trap (at the top side of the sample). (b) and (c) Elemental maps for Si and Cr, respectively, taken in the area outlined by yellow dashed line in (a).    \\u003c\/em\\u003e\\u003c\/em\\u003e\",\"width\":0} \/--><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eViscous EffeCTs On Raman-based elasto-thermobarometry (VECTOR): a field, mechanical and diffusion study of mineral inclusions entrapped under a wide range of metamorphic conditions\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the DFG and the National Science Centre (PL), 2024-2026\\u003cbr\/\\u003eIn collaboration with Prof. Dr. J. Szczepa\u0144ski (Uni. Wroclaw) and Prof. Dr. M. D\u0105browski (Polish Geol. Inst.)\",\"slug\":\"strongviscous-effects-on-raman-based-elasto-thermobarometry-vector-a-field-mechanical-and-diffusion-study-of-mineral-inclusions-entrapped-under-a-wide-range-of-metamorphic-conditions-strong-brfunded-by-the-the-dfg-and-the-national-science-centre-pl-2024-2026brin-collaboration-with-prof-dr-j-szczepanski-uni-wroclaw-and-prof-dr-m-dabrowski-polish-geol-inst\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">Recent advancements like Raman spectroscopy-based elasto-thermobarometry offer a new way to estimate the re-equilibration conditions in a rock's history. However, high-temperature irreversible deformation (viscous creep) has been identified to compromise the integrity of minerals' elastic properties, affecting their ability to retain residual pressure in inclusions. The project aims to develop a new method to quantify the impact of viscous creep on mineral inclusions' capacity to hold residual pressure, addressing a gap in systematic studies on this issue. Through integrating field data, analytical measurements, and numerical modeling of re-equilibration processes at the mineral level, this project seeks to quantitatively assess the effects of viscous creep and refine the accuracy of determining metamorphic conditions using Raman thermobarometry.   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"right\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15028},\"caption\":\"\\u003cem\\u003e\\u003cem\\u003eTimescale predictions for the exhumation of host-inclusion systems. The predictions are based on the numerical models of temperature-dependent viscoelastic relaxation (see Zhong, \\u003cstrong\\u003eMoulas\\u003c\/strong\\u003e, Taj\u010dmanov\u00e1 (2018) for more details). \\u003c\/em\\u003e\\u003c\/em\\u003e\",\"width\":0} \/--><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eA combination of petrological and joint chemical-mechanical inversion approaches to unravel deep geodynamic processes\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the DFG, 2024-2026\\u003cbr\/\\u003eIn collaboration with Dr. I. Ibragimov (Uni. Mainz)\",\"slug\":\"stronga-combination-of-petrological-and-joint-chemical-mechanical-inversion-approaches-to-unravel-deep-geodynamic-processes-strong-brfunded-by-the-the-dfg-2024-2026brin-collaboration-with-dr-i-ibragimov-uni-mainz\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">Metamorphism involves the recrystallization of rocks under high temperatures, subjecting them to various pressure and temperature conditions that lead to chemical and mechanical changes in their structure. As metamorphic rocks are brought to the surface, they often retain \"frozen\" evidence of these processes due to the rapid cooling they undergo, preserving high-temperature traces like chemically zoned crystals and stresses within mineral inclusions. Recent advancements in diffusion modeling and Raman elastic barometry have enhanced our understanding of these changes in natural rocks. This study aims to develop inverse models that could jointly infer the mechanical and chemical relaxation of metamorphic textures. Such models can be corroborated using geodynamic models that predict the P-T evolution of rocks. Focusing on metamorphic rocks, the approach seeks to quantify the slow, often imperceptible metamorphic processes that occur under the Earth's surface (see for example publication numbers <em>Ibragimov, Kiss, <strong>Moulas<\/strong>, (2024)<\/em> and <em>Schorn, <strong>Moulas<\/strong>, St\u00fcwe (2024)<\/em> for more details).     <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"right\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15032},\"caption\":\"\\u003cem\\u003e\\u003cem\\u003e\\u003cem\\u003eGeodynamic simulation of lithospheric convergence and continental subduction. The different rock units move through space and experience a variety of conditions. Thermally-activated processes such as solid-state mineral diffusion and viscous relaxation (creep) will occur in the deforming metamorphic rocks depending on the different paths taken by the rocks. The forward simulation of such processes will lead to a better understanding of the integrated geological data.   \\u003c\/em\\u003e\\u003c\/em\\u003e\\u003c\/em\\u003e\",\"width\":0} \/--><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eUncertain Nonlinearities in Groundwater Flow Models\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the M3ODEL Institute and RWTH Aachen, 2020-2025\\u003cbr\/\\u003eIn collaboration with Prof. Dr. M. Bachmayr (Applied Mathematics \u2013 RWTH Aachen)\\u003cbr\\u003e  \",\"slug\":\"stronguncertain-nonlinearities-in-groundwater-flow-models-strong-brfunded-by-the-m3odel-institute-and-rwth-aachen-2020-2025brin-collaboration-with-prof-dr-m-bachmayr-applied-mathematics-rwth-aachenbr\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The fluid flow in porous rocks is governed by complex and non-linear Partial Differential Equations (PDEs). In this project we are investigating the solvability and the behavior of non-linear porous-flow equations. These equations describe the fluid flow within deforming rocks. In particular, the complex volumetric rheology of rocks is investigated. The results of this study have many implications for energy applications that include the integrity and the permeability evolution of reservoir rocks.    <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"center\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":14893},\"caption\":\"\\u003cem\\u003ePorosity evolution (top row) and effective pressure evolution (bottom row) during compaction-driven fluid flow. The computational grid on the right spans the whole space-time domain. Figure courtesy of S. Boisser\u00e9e.  \\u003c\/em\\u003e\",\"width\":0} \/--><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eGrain-scale pressure variations in metamorphic rocks\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the M3ODEL Institute and the Alexander von Humboldt Foundation, 2020-2024\\u003cbr\/\\u003eIn collaboration with Dr. M. Mazzucchelli (Uni. Lausanne), \\u0026 Prof. Y. Podladchikov (Uni. Lausanne)\\u003cbr\\u003e\",\"slug\":\"stronggrain-scale-pressure-variations-in-metamorphic-rocks-strong-brfunded-by-the-m3odel-institute-and-the-alexander-von-humboldt-foundation-2020-2024brin-collaboration-with-dr-m-mazzucchelli-uni-lausanne-prof-y-podladchikov-uni-lausannebr\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">Metamorphic rocks are always deformed when recrystallized. Even in the absence of far-field deformation, the volumetric thermoelastic strains can lead to the development of GPa-level stresses at the mineral scale. For this reason, we develop new mechanical models that allow the quantification of the deformation in composite materials such as rocks. Such models are tested using spectroscopic techniques (e.g. Raman Spectroscopy) and can provide insightful information regarding the development of residual stresses.   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"center\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15008},\"caption\":\"\\u003cem\\u003e\\u003cem\\u003eA: Schematic representation of the elasto-plastic zone that develops at a host-inclusion interface. B: stress distribution around a pressurized mineral inclusion (see \\u003cstrong\\u003eMoulas\\u003c\/strong\\u003e et al (2020), Pl\u00fcmper, Wallis, Teuling, \\u003cstrong\\u003eMoulas\\u003c\/strong\\u003e  \\u003c\/em\\u003e\\u003c\/em\\u003e\\u003cem\\u003eet al. (2022) and \\u003cstrong\\u003eMoulas\\u003c\/strong\\u003e et al (2023)\\u003cem\\u003e for more details).\\u003c\/em\\u003e \\u003c\/em\\u003e\",\"width\":0} \/--><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n\n<!-- wp:jgu\/accordion-item {\"title\":\"\\u003cstrong\\u003eThermodynamic equilibrium and stress evolution of metamorphic rocks\\u003c\/strong\\u003e\\u003cbr\/\\u003eFunded by the M3ODEL institute, the Alexander von Humboldt foundation (2020-2023) and the University of Lausanne (2024-..)\\u003cbr\/\\u003eIn collaboration with Dr. M. Mazzucchelli (Uni. Lausanne), Prof. Dr. S. Schmalholz (Uni. Lausanne) \\u0026 Prof. Dr. T. Speck (Uni. Stuttgart)\",\"slug\":\"strongthermodynamic-equilibrium-and-stress-evolution-of-metamorphic-rocks-strong-brfunded-by-the-m3odel-institute-the-alexander-von-humboldt-foundation-2020-2023-and-the-university-of-lausanne-2024-brin-collaboration-with-dr-m-mazzucchelli-uni-lausanne-prof-dr-s-schmalholz-uni-lausanne-prof-dr-t-speck-uni-stuttgart\"} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The development of stresses in minerals affects their energy. As a result, the stability of metamorphic mineral assemblages does not depend on a simple \"pressure\" value and more complex theories are needed. In this research direction, we investigate the thermodynamic equilibrium of stressed rocks by means of:  <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\">i) deformation experiments corroborated by thermomechanical simulations<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">ii) hydro-chemo-mechanical modeling (multiphase flow equations)<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\">iii) classical molecular dynamics simulations<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">Our results can be used to create predictive models that can account for the effects of deformation on mineral reactions (see <em>Cionoiu, <strong>Moulas<\/strong>, Taj\u010dmanov\u00e1 (2019)<\/em>, <em>Schmalholz, <strong>Moulas<\/strong> et al. (2020), Cionoiu, <strong>Moulas<\/strong>, St\u00fcnitz, Taj\u010dmanov\u00e1 (2022) <\/em>, <em>Schmalholz,<strong> Moulas,<\/strong> R\u00e4ss, M\u00fcntener<\/em>, <em>(2023)<\/em> and <em>Mazzucchelli, <strong>Moulas,<\/strong> Kaus, Speck, (2024)<\/em> for more details).<\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:group {\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"flex\",\"orientation\":\"vertical\",\"justifyContent\":\"right\"}} -->\n<div class=\"wp-block-group\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:spacer {\"height\":\"55px\",\"style\":{\"layout\":{\"flexSize\":\"55px\",\"selfStretch\":\"fixed\"}}} -->\n<div style=\"height:55px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:jgu\/image {\"align\":\"right\",\"image\":{\"url\":null,\"id\":15020},\"caption\":\"\\u003cem\\u003eExample of a molecular dynamics simulation of the coexistence of a stressed solid with a melt of the same composition (see publication [38] for more details)\\u003c\/em\\u003e\",\"width\":0} \/-->\n\n<!-- wp:spacer {\"height\":\"9px\",\"style\":{\"layout\":{\"flexSize\":\"9px\",\"selfStretch\":\"fixed\"}}} -->\n<div style=\"height:9px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer --><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/accordion-item -->\n<!-- \/wp:jgu\/accordion -->\n\n<!-- wp:group {\"metadata\":{\"name\":\"Bidergalerie Arbeitsgruppe\"},\"align\":\"wide\",\"layout\":{\"type\":\"constrained\"}} -->\n<div class=\"wp-block-group alignwide\"><!-- wp:jgu\/heading {\"color\":\"default\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"h1\",\"tag\":\"h2.h1\"},\"heading\":\"\\u003cbr\/\\u003e\",\"metadata\":{\"name\":\"Bildergalerie Institut\"},\"className\":\"\"} \/-->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"33.33%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:33.33%\"><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"80%\",\"layout\":{\"type\":\"default\"}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:80%\"><!-- wp:jgu\/image-gallery {\"images\":[{\"url\":null,\"id\":15112},{\"url\":null,\"id\":14903},{\"url\":null,\"id\":15347},{\"url\":null,\"id\":15344},{\"url\":null,\"id\":15341},{\"url\":null,\"id\":15350},{\"url\":null,\"id\":15352}],\"thumbsPosition\":\"bottom\"} \/--><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"33.34%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:33.34%\"><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><\/div>\n<!-- \/wp:group --><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"light\",\"metadata\":{\"name\":\"Team\"}} -->\n<div class=\"jgu-bgsection bg bg-light \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Team\",\"slug\":\"team\"} \/-->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Team\",\"className\":\"\"} \/-->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"257357\",\"organizationId\":976,\"roleId\":13,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Moulas, Univ.-Prof. Dr. Evangelos\",\"avatar\":{\"id\":25024,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Professor\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"evmoulas \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"phone-solid\",\"title\":\"\\u003ca href=\\u0022tel:+4961313924784\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003e+49 6131 39 24784\\u003c\/a\\u003e\",\"uuid\":\"1783508889771\",\"link\":{\"url\":\"tel:+4961313924784\"}} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/257357\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/257357\"}} \/-->\n<!-- \/wp:jgu\/contact-card -->\n\n<!-- wp:jgu\/button -->\n<!-- wp:jgu\/button-item {\"text\":\"Research profile E. Moulas\",\"icon\":\"user-check-solid\",\"link\":{\"url\":\"https:\/\/metamorphism.de\/\",\"linkTarget\":\"\",\"rel\":\"\",\"id\":\"https:\/\/metamorphism.de\/\",\"title\":\"https:\/\/metamorphism.de\/\",\"type\":\"link\",\"opensInNewTab\":true}} \/-->\n<!-- \/wp:jgu\/button --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"3305\",\"organizationId\":968,\"roleId\":16,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Helo, Dr. Christoph\",\"avatar\":{\"id\":25039,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Academic staff members\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"helo \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"phone-solid\",\"title\":\"\\u003ca href=\\u0022tel:+4961313924784\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003e+49 6131 39 27004\\u003c\/a\\u003e\",\"uuid\":\"1783508889771\",\"link\":{\"url\":\"tel:+4961313924784\"}} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/3305\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/3305\"}} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"337016\",\"organizationId\":976,\"roleId\":16,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Boisser\u00e9e, Dr. Simon\",\"avatar\":{\"id\":25036,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Academic staff members\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"boisseree \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/337016\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/337016\"}} \/-->\n<!-- \/wp:jgu\/contact-card -->\n\n<!-- wp:spacer {\"height\":\"45px\"} -->\n<div style=\"height:45px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:jgu\/button -->\n<!-- wp:jgu\/button-item {\"text\":\"Homepage\",\"icon\":\"user-check-solid\",\"link\":{\"url\":\" \\nhttps:\/\/boisseree.github.io\",\"opensInNewTab\":true}} \/-->\n<!-- \/wp:jgu\/button --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"12469\",\"organizationId\":976,\"roleId\":16,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Riel, Dr. Nicolas\",\"avatar\":{\"id\":25057,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Academic staff members\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"nriel \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/12469\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/12469\"}} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"100%\",\"metadata\":{\"name\":\"manuell\",\"blockVisibility\":false}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Schorn, Dr. Simon\",\"avatar\":{\"id\":15503,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Humboldt scholarship student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Metamorphic Processes\",\"uuid\":\"1773144984525\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"schorsim \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\",\"metadata\":{\"blockVisibility\":false}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"307071\",\"name\":\"Dimitri\",\"organizationId\":976,\"roleId\":42,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Moutzouris, Dimitrios\",\"avatar\":{\"id\":25071,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Doctoral candidate\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Metamorphic Processes\",\"uuid\":\"1773144984525\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"dimoutzo \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"phone-solid\",\"title\":\"\\u003ca href=\\u0022tel:+4961313930798\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003e+49 6131 39 30798\\u003c\/a\\u003e\",\"uuid\":\"1783508889771\",\"link\":{\"url\":\"tel:+4961313930798\"}} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/307071\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/307071\"}} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"9111\",\"organizationId\":976,\"roleId\":42,\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/contact-card {\"name\":\"Stroh, Annalena\",\"avatar\":{\"id\":25074,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"PhD Students\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"anstroh \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"external-link-alt-solid\",\"title\":\"\\u003ca href=\\u0022https:\/\/personen.uni-mainz.de\/person\/9111\\u0022 target=\\u0022_blank\\u0022 rel=\\u0022noreferrer noopener\\u0022\\u003eProfile\\u003c\/a\\u003e\",\"uuid\":\"1783508167564\",\"link\":{\"url\":\"https:\/\/personen.uni-mainz.de\/person\/9111\"}} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person {\"id\":\"291905\",\"organizationId\":810,\"roleId\":16,\"metadata\":{\"blockVisibility\":false}} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>MSc and BSc students<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"100%\",\"metadata\":{\"blockVisibility\":false}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Daubner, Diana\",\"avatar\":{\"id\":15568,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"MSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Metamorphic Processes\",\"uuid\":\"1773144984525\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"ddaubner\\u003cem\\u003e\\u003cstrong\\u003e \\u003c\/strong\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\",\"metadata\":{\"name\":\"manuell\",\"blockVisibility\":false}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"David, Jana\",\"avatar\":{\"id\":15188,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"MSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Metamorphic Processes\",\"uuid\":\"1773144984525\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"jdavid01 \\u003cem\\u003eat\\u003c\/em\\u003e uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Fe\u00dfler, Claudia\",\"avatar\":{\"id\":15569,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"MSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"cfessler \\u003cem\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Lamest, Stella\",\"avatar\":{\"id\":15142,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"MSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"slamest \\u003cem\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"100%\",\"metadata\":{\"name\":\"manuell\"}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Vakhitova, Katerina\",\"avatar\":{\"id\":15574,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"MSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"kvakhito \\u003cem\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\",\"metadata\":{\"blockVisibility\":false}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Klups, Melanie\",\"avatar\":{\"id\":15587,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"BSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Metamorphic Processes\",\"uuid\":\"1773144984525\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"mklups \\u003cem\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/contact-card {\"name\":\"Lotz, Katharina\",\"avatar\":{\"id\":15583,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"BSc student\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"envelope-solid\",\"title\":\"klotz01 \\u003cem\\u003eat\\u003c\/em\\u003e students.uni-mainz.de\\u003cbr\\u003e\",\"uuid\":\"1773145031183\"} \/-->\n<!-- \/wp:jgu\/contact-card --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>Former group members<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/list -->\n<ul class=\"styled-list hyphenation\"><!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eDoctoral candidates \\u0026 academic staff members\\u003c\/strong\\u003e\",\"uuid\":\"1783587086848\",\"link\":{\"url\":null}} -->\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cbr\\u003eDr. Iskander Ibragimov (Utrecht University)\",\"uuid\":\"1783587152405\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Dr. Mattia Mazzucchelli (University of Lausanne)\",\"uuid\":\"1783587152405\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Dr. Dimitrios Moutzouris (Goethe University Frankfurt)\",\"uuid\":\"1783587564908\"} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Dr. Simon Schorn (RHI Magnesita)\",\"uuid\":\"1783587564908\"} \/-->\n<!-- \/wp:jgu\/list-item -->\n\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cstrong\\u003eBSc \\u0026 MSc students\\u003c\/strong\\u003e\",\"uuid\":\"1783587086848\",\"link\":{\"url\":null}} -->\n<!-- wp:jgu\/list-item {\"title\":\"\\u003cbr\\u003eDiana Daubner (Baugrundinstitut Franke-Mei\u00dfner und Partner GmbH) \",\"uuid\":\"1783587152405\",\"link\":{\"url\":null}} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Jana David (Baugrundinstitut Franke-Mei\u00dfner und Partner GmbH) \",\"uuid\":\"1783587564908\"} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Melanie Klups\",\"uuid\":\"1783587564908\"} \/-->\n\n<!-- wp:jgu\/list-item {\"title\":\"Clara Nuszer\",\"uuid\":\"1783587152405\",\"link\":{\"url\":null}} \/-->\n<!-- \/wp:jgu\/list-item --><\/ul>\n<!-- \/wp:jgu\/list --><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"white-dark-text\",\"metadata\":{\"name\":\"Labore\",\"blockVisibility\":false}} -->\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Laboratories\",\"slug\":\"laboratories\",\"className\":\"\"} \/-->\n\n<!-- wp:group {\"layout\":{\"type\":\"constrained\"}} -->\n<div class=\"wp-block-group\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":13577},\"caption\":\"Image size is 1280x722\"} \/--><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Laboratories\",\"className\":\"alignwide\"} \/-->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>Equipment<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/tabs {\"layout\":{\"type\":\"flex\",\"flexWrap\":\"nowrap\",\"justifyContent\":\"left\",\"orientation\":\"vertical\"}} -->\n<!-- wp:jgu\/tabs-item {\"title\":\"GC-IRMS (Finnigan MAT 253)\",\"slug\":\"gc-irms-finnigan-mat-253\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">CF-IRMS stands for Continuous Flow Isotope Ratio Mass Spectrometry. It is an analytical method from isotope geochemistry and analytical chemistry that is used to determine the ratio of stable isotopes of an element in a sample with very high precision, for example carbon (<sup>13<\/sup>C\/<sup>12<\/sup>C), nitrogen (<sup>15<\/sup>N\/<sup>14<\/sup>N), or oxygen (<sup>18<\/sup>O\/<sup>16<\/sup>O). <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12869}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"Gasbench (Finnigan Gasbench II)\",\"slug\":\"gasbench-finnigan-gasbench-ii\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">CF-IRMS stands for Continuous Flow Isotope Ratio Mass Spectrometry. It is an analytical method from isotope geochemistry and analytical chemistry that is used to determine the ratio of stable isotopes of an element in a sample with very high precision, for example carbon (<sup>13<\/sup>C\/<sup>12<\/sup>C), nitrogen (<sup>15<\/sup>N\/<sup>14<\/sup>N), or oxygen (<sup>18<\/sup>O\/<sup>16<\/sup>O). <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12869}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"TC-EA (Finnigan TC-EA)\",\"slug\":\"tc-ea-finnigan-tc-ea\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">TC-EA stands for Thermal Combustion Elemental Analyzer. It is used to reduce various oxygen-containing substances such as phosphates, waters, or cellulose to carbon monoxide at high temperatures of 1450\u00b0C in a glassy carbon reactor, the oxygen isotope composition of which is then measured in a CF-IRMS.  <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong> <\/p>\n<!-- \/wp:paragraph -->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"Flash EA (Vario EL)\",\"slug\":\"flash-ea-vario-el\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">EA stands for Elemental Analyzer. With this device, organic substances such as soil, leaves, hair, collagen, cellulose, or biominerals weighed into tin capsules are oxidized at 1050\u00b0C in a cobalt oxide-containing reactor with the addition of oxygen. A downstream reactor with elemental copper eliminates excess oxygen or reduces nitrogen oxides to nitrogen gas. Using a connected CF-IRMS, the isotope ratios of stable isotopes of carbon (<sup>13<\/sup>C\/<sup>12<\/sup>C), nitrogen (<sup>15<\/sup>N\/<sup>14<\/sup>N), or sulfur (<sup>34<\/sup>S\/<sup>32<\/sup>S) in CO<sub>2<\/sub> or N<sub>2<\/sub> can be determined with an accuracy of a few tenths of a per mil.   <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12886}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"ICP-OES (Spectro Ciros Vision)\",\"slug\":\"icp-oes-spectro-ciros-vision\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">ICP-OES is an analytical method from analytical chemistry for determining the elemental composition of a sample. In an Ar plasma, the atoms of the elements are excited and emit characteristic light radiation. This emitted radiation is separated by wavelength and measured in an optical emission spectrometer. Since each element has a typical emission spectrum, the elements present can be identified and their concentrations determined. ICP-OES is frequently used in environmental analysis, materials science, geochemistry, and food analysis to quickly and simultaneously determine metals and trace elements in a sample.    <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Prof. Dr. Thomas T\u00fctken<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12874}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"HPLC-MS (Aligent 1260 Infinity II, Agilent MSD, ESI ion source)\",\"slug\":\"hplc-ms-aligent-1260-infinity-ii-agilent-msd-esi-ion-source\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">LC-MS with electrospray ionization (ESI) is a powerful analytical method for investigating and determining organic compounds in complex samples. First, the components of the sample are separated from one another by a liquid chromatograph (LC). The eluting compounds then enter an electrospray ionization source, where a fine, electrically charged <g id=\"gid_0\">spray <\/g>is generated from the liquid phase. As the solvent evaporates, charged molecular ions are formed and then transferred to the mass spectrometer. There, the ions are separated and detected according to their mass-to-charge ratio (m\/z). Due to the gentle ionization, this technique is particularly suitable for polar and thermally sensitive molecules. It is therefore frequently used in areas such as pharmaceutical and environmental analysis, food analysis, and biochemical and metabolomic research, especially for the rapid and straightforward determination of dissolved substances such as proteins, nucleic acids, dyes, or metal ions.      <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12875}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"SEM (Phenom PRO Desktop SEM (G3) \",\"slug\":\"sem-phenom-pro-desktop-sem-g3\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The 3rd-generation Phenom PRO offers powerful imaging capabilities in a compact desktop format. It is optimized for users who require precise results with maximum throughput. The ProSuite platform extends the Phenom PRO with specialized analysis tools to extract quantitative data directly from SEM images. In addition, the <strong>Leica EM ACE200<\/strong> sample coater enables fully automated sputter coating with platinum (Pt) and gold\/palladium (Au\/Pd) for optimal conductivity.   <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"small\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-small-font-size\">Analysis: Voltage levels of 5 kV and 10 kV to optimize material contrast and surface details.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"small\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-small-font-size\">Imaging: Resolution up to 17 nm at magnifications from 20x to 100,000x.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"small\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-small-font-size\">Electron source: High-intensity CeB6 source for increased brightness and detail resolution.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"small\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-small-font-size\">Workflow: Sample exchange and image display in  30 seconds.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"small\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-small-font-size\">Navigation: Combined optical color camera and electron optics for intuitive sample positioning.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12877}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"PrepFast MC (ESI)\",\"slug\":\"prepfast-mc-esi\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>PrepFAST<\/strong> from Elemental Scientific (ESI) is used to automate sample preparation for MC-ICP-MS isotope analysis of heavy isotopes. It enables automated ion-chromatographic separation of the elements Ca and Sr from the matrix for isotope analysis. For this purpose, the sample must first be dissolved in HCl.  <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:tuetken@uni-mainz.de\">Prof. Dr. Thomas T\u00fctken<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12880}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"Cryomill (Retsch)\",\"slug\":\"cryomill-retsch\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The Cryomill is a specialized ball mill used to gently grind soft tissue or biomineralizates to an analytical fineness while cooling the grinding jar and material with liquid nitrogen.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:tuetken@uni-mainz.de\">Prof. Dr. Thomas T\u00fctken<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12907}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"Micromill (New Wave Research)\",\"slug\":\"micromill-new-wave-research\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The Micromill enables the sampling of small powder samples (\u00b5g quantities) from rocks or (bio-)minerals with high spatial resolution for elemental or isotope analyses. Typically, accretionary carbonate proxy archives such as shells, otoliths, or speleothems are sampled. <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:tuetken@uni-mainz.de\">Prof. Dr. Thomas T\u00fctken<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12908}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"GC-C-IRMS (Trace 2000 GC, Delta V IRMS)\",\"slug\":\"gc-c-irms-trace-2000-gc-delta-v-irms\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">GC-C-IRMS (gas chromatography\u2013combustion\u2013isotope ratio mass spectrometry) is an analytical method for determining stable isotope ratios of individual compounds within a sample. With this technique, the individual components of a sample are first separated from one another using a gas chromatograph (GC). The separated compounds are then converted into simple gases such as CO\u2082 or N\u2082 in a combustion furnace (combustion interface). These gases are subsequently analyzed in an isotope ratio mass spectrometer (IRMS), which determines the ratios of stable isotopes (e.g., \u00b9\u00b3C\/\u00b9\u00b2C or \u00b9\u2075N\/\u00b9\u2074N) with high precision. The method is used in various scientific fields, including environmental research, food analysis, forensics, and geochemistry. In particular, it is used to investigate sources, origin, and biogeochemical processes of organic compounds.     <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact person: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12890}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"UV-VIS (Spectroquant Pharo 300 Merck)\",\"slug\":\"uv-vis-spectroquant-pharo-300-merck\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">UV\/Vis Spectroscopy is used to determine and quantify substances in solution based on their light absorption in the ultraviolet and visible wavelength range. A sample is irradiated with light in the UV and visible range. Certain molecules absorb light at characteristic wavelengths, causing electrons to be excited to higher energy levels. The attenuation of light intensity is measured and can be used to determine the concentration of a substance. Application areas include chemical analysis, environmental analysis, food analysis, and biochemical research, particularly for the rapid and simple determination of dissolved substances such as proteins, nucleic acids, dyes, or metal ions.    <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12892}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"IsoMet Low Speed Precision Cutter\",\"slug\":\"isomet-low-speed-prazesionstrenner\"} -->\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">The IsoMet saw is used for precise and material-preserving cutting of smaller hard tissue or rock samples with water-cooled diamond-tipped saw blades with minimal sample loss.<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Contact persons: <a href=\"mailto:schoeneb@uni-mainz.de\">Prof. Dr. B. Sch\u00f6ne<\/a>, <a href=\"mailto:mausm@uni-mainz.de\">Michael Maus<\/a><\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":12904}} \/-->\n<!-- \/wp:jgu\/tabs-item -->\n<!-- \/wp:jgu\/tabs -->\n\n<!-- wp:group {\"metadata\":{\"name\":\"Bidergalerie Arbeitsgruppe\"},\"align\":\"wide\",\"layout\":{\"type\":\"constrained\"}} -->\n<div class=\"wp-block-group alignwide\"><!-- wp:jgu\/heading {\"color\":\"default\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"h1\",\"tag\":\"h2.h1\"},\"heading\":\"\\u003cbr\/\\u003e\",\"metadata\":{\"name\":\"Bildergalerie Institut\"},\"className\":\"\"} \/-->\n\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"100%\",\"layout\":{\"type\":\"default\"}} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/image-gallery {\"images\":[{\"url\":null,\"id\":12890},{\"url\":null,\"id\":12886},{\"url\":null,\"id\":12880},{\"url\":null,\"id\":12874},{\"url\":null,\"id\":12875},{\"url\":null,\"id\":12877},{\"url\":null,\"id\":12869},{\"url\":null,\"id\":12908},{\"url\":null,\"id\":12907},{\"url\":null,\"id\":12904},{\"url\":null,\"id\":12892}],\"thumbsPosition\":\"bottom\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><\/div>\n<!-- \/wp:group --><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"white-dark-text\",\"metadata\":{\"name\":\"Lehre\"}} -->\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Teaching\",\"slug\":\"teaching\"} \/-->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Teaching\",\"className\":\"alignwide\"} \/-->\n\n<!-- wp:jgu\/image {\"align\":\"center\",\"image\":{\"url\":null,\"id\":15134},\"imgWidth\":1281,\"width\":0} \/-->\n\n<!-- wp:spacer {\"height\":\"30px\"} -->\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"align\":\"wide\",\"style\":{\"shadow\":\"var:preset|shadow|natural\"},\"layout\":{\"type\":\"constrained\"}} -->\n<div class=\"wp-block-group alignwide\" style=\"box-shadow:var(--wp--preset--shadow--natural)\"><!-- wp:jgu\/tabs {\"metadata\":{\"name\":\"Lehrveranstaltungen\"}} -->\n<!-- wp:jgu\/tabs-item {\"title\":\"BSc courses\",\"slug\":\"bsc-veranstaltungen\",\"metadata\":{\"name\":\"BSc Geowissenschaften\"}} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Compulsory Module Endogenous Geology<\/strong> - M.09.065.010.B<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list {\"fontSize\":\"small\"} -->\n<ul class=\"wp-block-list has-small-font-size\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Fundamentals of Endogenous Geology - 09.065.011.B<\/strong> | C. Helo<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Petrological internship (endogenous) - 09.065.012.B<\/strong> | C.Helo<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Field Internship (endogenous) - 09.065.013.B<\/strong> | C. Helo, K. Seelos <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Compulsory Module Petrology<\/strong> - M.09.065.062.B (together with Petrology working group)<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Petrology of magmatic and metamorphic rocks - 09.065.062.B  <\/strong> | R. Botcharnikov, E. Moulas<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Petrology of magmatic and metamorphic rocks practice class <\/strong>  - <strong>09.065.063.B<\/strong> | R. Botcharnikov, S. Buhre, E. Moulas <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Compulsory Module Geological Fieldwork<\/strong> - M.09.065.050.B <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Day Excursion 1 - 09.065.053.B<\/strong> | S. Buhre, C. Helo<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Day Excursion 2 - 09.065.054.B<\/strong> | R. Botcharnikov, E. Moulas<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Elective Module Dynamic Processes and Data Science<\/strong> - M.09.065.220.B <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Dynamic Processes and Data Science - 09.065.221.B<\/strong> | R. Botcharnikov, B. Kaus, E. Moulas <\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Dynamic Processes and Data Science - 09.065.222.B<\/strong> | B. Kaus, E. Moulas <\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li> <strong>Big Data and Machine Learning<\/strong> - <strong>09.065.223.B<\/strong> | E. Moulas <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Extracurricular Events<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Anatomy of rock-forming minerals<\/strong> | C. Helo<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>BSc\/MSc Project seminar<\/strong> | C. Helo<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:spacer {\"height\":\"30px\"} -->\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":15188}} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/tabs-item -->\n\n<!-- wp:jgu\/tabs-item {\"title\":\"MSc courses\",\"slug\":\"msc-veranstaltungen\",\"metadata\":{\"name\":\"MSc Geowissenschaften\"}} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":15223}} \/--><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Elective Module Petrogenesis<\/strong> - M.09.065.520<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Metamorphic Petrogenesis - 09.065.M522<\/strong> | E. Moulas <\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Volcanology (thermodynamic aspects) - 09.065.M522<\/strong> | C. Helo <\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>MSc Petrology Project - 09.065.M522<\/strong> | R. Botcharnikov, S. Buhre, C. Helo, E. Moulas<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Elective Module Dynamics of the Lithosphere<\/strong> - M.09.065.505<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Orogenic Systems - 09.065.M533<\/strong> | R. Botcharnikov, J. Castro, E. Moulas <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Elective Module Geodynamical and Petrological Methods<\/strong> - M.09.065.570<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Mineral Equilibria Modelling - 09.065.M572<\/strong> | E. Moulas <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Compulsory Module Field<\/strong> - M.09.065.500<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Field Course Exogenous Geology - 09.065.M503<\/strong> | F. Hawemann, C. Helo<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\",\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-normal-font-size\"><strong>Extracurricular Events<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>Anatomy of rock-forming minerals<\/strong> | C. Helo<\/li>\n<!-- \/wp:list-item -->\n\n<!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><strong>BSc\/MSc Project seminar<\/strong> | C. Helo<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:spacer {\"height\":\"30px\"} -->\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/tabs-item -->\n<!-- \/wp:jgu\/tabs --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:jgu\/image-gallery {\"images\":[{\"url\":null,\"id\":15151},{\"url\":null,\"id\":15148},{\"url\":null,\"id\":15139},{\"url\":null,\"id\":15136},{\"url\":null,\"id\":15142},{\"url\":null,\"id\":15145,\"darkBackground\":true}],\"withThumbs\":false,\"thumbsPosition\":\"top\",\"perPage\":2} \/--><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"dark\",\"metadata\":{\"name\":\"Software\"}} -->\n<div class=\"jgu-bgsection bg bg-dark \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Software\",\"slug\":\"software\",\"className\":\"\"} \/-->\n\n<!-- wp:jgu\/heading {\"color\":\"default\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Software\",\"className\":\"alignwide\"} \/-->\n\n<!-- wp:group {\"layout\":{\"type\":\"constrained\",\"justifyContent\":\"center\"}} -->\n<div class=\"wp-block-group\"><!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><strong>2026<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[14]<\/strong> <strong>Moulas E<\/strong> (2026). Numerical Modelling of Geological Processes, with emphasis on Geochemistry, Petrology and Geochronology (Workshop Lecture Notes and Codes). Zenodo. doi: <a href=\"https:\/\/doi.org\/10.5281\/zenodo.18413414\">10.5281\/zenodo.18413414<\/a>.   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"60px\"} -->\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><strong>2025<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[13]<\/strong> <strong>Moulas E<\/strong> (2025) TEMP2D: A simple thermo-kinematic model for rock exhumation in 2-D. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15830073\">10.5281\/zenodo.15830072<\/a>   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[12]<\/strong> Stroh A, Aellig P, <strong>Moulas E<\/strong> (2025) AnStroh\/MovingBoundaryMinerals.jl: v0.1.0. (A Julia package for the calculation of chemical diffusion in growing crystals). Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15546347\">10.5281\/zenodo.15535732<\/a>    <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[11]<\/strong> Riel N, Kaus B, de Montserrat A, <strong>Moulas E<\/strong>, Green E, Dominguez H (2025) An unconstrained formulation for complex solution phase minimization (Codes). Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/13982544\">10.5281\/zenodo.13982543<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[10]<\/strong> Porkol\u00e1b K, <strong>Moulas E<\/strong>, Schmalholz SM (2025) Code and thermodynamic data for a 2D hydro-mechanical-chemical model of antigorite dehydration. Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/14202518\">10.5281\/zenodo.14202517<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"60px\"} -->\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><strong>2024<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[9]<\/strong> Boisser\u00e9e S, <strong>Moulas E<\/strong>, Bachmayr M (2024) Fluid flow channeling and mass transport with discontinuous porosity distribution (Julia code for hydromechanical solver and chemical postprocessing). Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/15758079\">10.5281\/zenodo.13986982<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[8]<\/strong> Schorn S, <strong>Moulas E<\/strong> (2024) ZirTiDiS: an implicit finite difference code for the calculation of apparent Zr-in-Titanite (ZiT) temperatures. Zenodo. doi:<a href=\"https:\/\/zenodo.org\/records\/11184086\">10.5281\/zenodo.11184085<\/a>   <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[7]<\/strong> Stroh A, <strong>Moulas E<\/strong>, Botcharnikov R (2024) FIDDO: FInite Difference Diffusion in Olivine. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/10964860\">10.5281\/zenodo.10964859<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[6]<\/strong> <strong>Moulas E<\/strong>, Schorn S (2024) T1dH: A 1-d code for the calculation of Heat conduction with Earth Science Applications. Zenodo. doi: <a href=\"https:\/\/zenodo.org\/records\/11046566\">10.5281\/zenodo.11046565<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"60px\"} -->\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><strong>2023<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[5] Moulas E<\/strong> (2023) Numerical Modelling of Chemical Diffusion in Petrology and Geochemistry (Workshop Lecture Notes). Zenodo. <a href=\"https:\/\/zenodo.org\/records\/10053579\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.10047582<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[4] Moulas E<\/strong> (2023) GDIFF: a Finite Difference code for the calculation of multicomponent diffusion in garnet. Zenodo. <a href=\"https:\/\/zenodo.org\/record\/7940212\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.7805989<\/a>  <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"60px\"} -->\n<div style=\"height:60px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><strong>2022<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[3] Moulas E<\/strong>, Brandon MT (2022) KADMOS: a Finite Element code for the calculation of apparent K-Ar ages in minerals. Zenodo. <a href=\"https:\/\/zenodo.org\/record\/7358138#.ZDBc-tJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.7358138<\/a> <\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[2]<\/strong> Cionoiu S, <strong>Moulas E<\/strong>, Taj\u010dmanov\u00e1 L (2022) Local variation of mechanical parameters in (Griggs-type) viscous deformation experiments (Matlab code). <a href=\"https:\/\/zenodo.org\/record\/6951760#.ZDBdVNJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi:10.5281\/zenodo.6951759<\/a><\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:spacer {\"height\":\"25px\"} -->\n<div style=\"height:25px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:group {\"layout\":{\"type\":\"grid\",\"columnCount\":8,\"minimumColumnWidth\":null}} -->\n<div class=\"wp-block-group\"><!-- wp:paragraph {\"style\":{\"layout\":{\"columnSpan\":1,\"rowSpan\":1}}} -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"style\":{\"layout\":{\"rowSpan\":1,\"columnSpan\":7}},\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>[1]<\/strong> <strong>Moulas E<\/strong>, Kaus B, Jamtveit B (2022) Dynamic Pressure Variations in the Lower Crust Caused by Localized Fluid-Induced Weakening (LaMEM input files). <a href=\"https:\/\/zenodo.org\/record\/6538290#.ZDBdttJBwSM\" target=\"_blank\" rel=\"noreferrer noopener\">doi: 10.5281\/zenodo.6538290<\/a><\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:group --><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph --><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"dark\",\"metadata\":{\"name\":\"Publikationen\"}} -->\n<div class=\"jgu-bgsection bg bg-dark \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Publications\",\"slug\":\"publications\",\"className\":\"\"} \/-->\n\n<!-- wp:jgu\/heading {\"color\":\"default\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Publications\",\"className\":\"\"} \/-->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":15089},\"metadata\":{\"blockVisibility\":false}} \/-->\n\n<!-- wp:jgu\/fis {\"user\":\"evmoulas\"} \/--><\/div><\/div>\n<!-- \/wp:jgu\/section -->","_links":{"self":[{"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/pages\/21755","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/users\/1931"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/comments?post=21755"}],"version-history":[{"count":6,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/pages\/21755\/revisions"}],"predecessor-version":[{"id":25138,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/pages\/21755\/revisions\/25138"}],"up":[{"embeddable":true,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/pages\/21238"}],"wp:attachment":[{"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/media?parent=21755"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/categories?post=21755"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.geowiss.uni-mainz.de\/en\/wp-json\/wp\/v2\/tags?post=21755"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}