{"id":21704,"date":"2026-03-17T10:03:00","date_gmt":"2026-03-17T09:03:00","guid":{"rendered":"https:\/\/www.geowiss.uni-mainz.de\/institut-fuer-geowissenschaften\/geoarchaeologie\/"},"modified":"2026-05-05T16:31:12","modified_gmt":"2026-05-05T14:31:12","slug":"geoarchaeologie","status":"publish","type":"page","link":"https:\/\/www.geowiss.uni-mainz.de\/en\/institut-fuer-geowissenschaften\/geoarchaeologie\/","title":{"rendered":"Geoarchaeology"},"content":{"rendered":"<jgu-base-anchornavigation react-props=\"{\n    &quot;align&quot;: &quot;wide&quot;,\n    &quot;theme&quot;: &quot;white&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;: 9757,\n        &quot;url&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1.jpg&quot;,\n        &quot;caption&quot;: &quot;Sinterablagerung Aqua Marcia Rom&quot;,\n        &quot;title&quot;: &quot;marcia1&quot;,\n        &quot;width&quot;: 2476,\n        &quot;height&quot;: 1134,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1.jpg 2476w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1-300x137.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1-1024x469.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1-768x352.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1-1536x703.jpg 1536w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2025\\\/10\\\/marcia1-2048x938.jpg 2048w&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;Geoarchaeology&lt;\\\/strong&gt;&quot;,\n    &quot;excerpt&quot;: &quot;&lt;strong&gt;We reconstruct the function of ancient water supply systems such as aqueducts based on the composition of carbonate deposits, using geological methods in antiquity.&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;Geoarchaeology&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-9d6595d7 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\">Geoarchaeology is the application of geological knowledge to archaeological sites. The Geoarchaeology Work Group in Mainz focuses primarily on the ancient culture of the Mediterranean region, particularly the Roman period. We specialize in researching ancient water supply systems such as aqueducts and the application of geological methods in antiquity. Our main task is the investigation of calcareous deposits in ancient aqueducts, water mills, lifting installations, and baths using fabric analysis and geochemical procedures. From these deposits, we obtain information about ancient water management, societal changes, the environment and climate of antiquity, as well as earthquakes. In addition to this core area, we research the use of building stones and quarrying operations in antiquity, the properties of Roman concrete, and attempt to reconstruct the understanding of geology and engineering among prospectors, architects, and engineers of antiquity.     <\/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\\\/Aqua-Marcia_Rome.jpeg&quot;,\n        &quot;id&quot;: 13031,\n        &quot;caption&quot;: &quot;Aqua Marcia Rom&quot;,\n        &quot;title&quot;: &quot;Aqua Marcia_Rome&quot;,\n        &quot;width&quot;: 1600,\n        &quot;height&quot;: 1200,\n        &quot;srcset&quot;: 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 &quot;color&quot;: &quot;red&quot;\n}\"><\/jgu-base-heading>\n\n\n<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\\\/Replica-of-a-Roman-saw-scaled.jpeg&quot;,\n        &quot;id&quot;: 14300,\n        &quot;caption&quot;: &quot;Nachbildung r\\u00f6mische S\\u00e4ge&quot;,\n        &quot;title&quot;: &quot;Replica of a Roman saw&quot;,\n        &quot;width&quot;: 2560,\n        &quot;height&quot;: 1920,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Replica-of-a-Roman-saw-scaled.jpeg 2560w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Replica-of-a-Roman-saw-300x225.jpeg 300w, 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class=\"align-\">\n    \n<\/jgu-base-image>\n\n\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/hygienische-bedingungen-in-pompejis-fruehen-baedern-waren-schlecht\/\"><strong>Hygienic conditions in Pompeii&#8217;s early baths were poor<\/strong><\/a> Calcareous deposits in wells, pipes, and bathing facilities provide insights into Pompeii&#8217;s ancient water supply<\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\"><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\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1.jpg&quot;,\n        &quot;id&quot;: 11575,\n        &quot;caption&quot;: &quot;Bad Pompeji&quot;,\n        &quot;title&quot;: &quot;09_geowissenschaften_pompeji_baeder_becken-1-scaled&quot;,\n        &quot;width&quot;: 2560,\n        &quot;height&quot;: 1920,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1.jpg 2560w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1-300x225.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1-1024x768.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1-768x576.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1-1536x1152.jpg 1536w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowissenschaften_pompeji_baeder_becken-1-scaled-1-2048x1536.jpg 2048w&quot;\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    \n<\/jgu-base-image><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/das-wassermanagement-des-antiken-arles\/\"><strong>The water management of ancient Arles<\/strong><\/a> Using carbonate fragments, researchers from Mainz, Oxford, and Innsbruck have deciphered the complex history of the aqueduct system of Arles<\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\"><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\\\/Aquaedukt-Arles.jpg&quot;,\n        &quot;id&quot;: 14345,\n        &quot;title&quot;: &quot;Aqu\\u00e4dukt Arles&quot;,\n        &quot;width&quot;: 1280,\n        &quot;height&quot;: 960,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Aquaedukt-Arles.jpg 1280w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Aquaedukt-Arles-300x225.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Aquaedukt-Arles-1024x768.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Aquaedukt-Arles-768x576.jpg 768w&quot;\n    },\n    &quot;caption&quot;: &quot;Aqueduct of Arles&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image>\n\n\n<p class=\"has-normal-font-size\"><\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/unbekannte-mikroorganismen-nutzten-marmor-und-kalkstein-als-lebensraum\/\"><strong>Unknown microorganisms used marble and limestone as habitat<\/strong><\/a> Unusual structures are noticeable in the rock of desert regions, whose origin has not been clarified<\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\"><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\\\/Mikroorganismien-im-Marmor.jpg&quot;,\n        &quot;id&quot;: 14347,\n        &quot;title&quot;: &quot;Mikroorganismien im Marmor&quot;,\n        &quot;width&quot;: 2560,\n        &quot;height&quot;: 1180,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor.jpg 2560w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor-300x138.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor-1024x472.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor-768x354.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor-1536x708.jpg 1536w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Mikroorganismien-im-Marmor-2048x944.jpg 2048w&quot;\n    },\n    &quot;caption&quot;: &quot;Marble sample from Namibia&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/karbonatschichten-eroeffnen-blick-in-die-roemerzeit\/\"><strong>Carbonate layers open a view into the Roman era<\/strong><\/a> Researchers reconstruct the developmental history of the water mills of Barbegal through carbonate deposits<\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\">\n<p class=\"has-big-font-size\"><\/p>\n\n\n<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\\\/Karbonatfragment-mit-Sinterlagen.jpg&quot;,\n        &quot;id&quot;: 14350,\n        &quot;title&quot;: &quot;Karbonatfragment mit Sinterlagen&quot;,\n        &quot;width&quot;: 2560,\n        &quot;height&quot;: 1642,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Karbonatfragment-mit-Sinterlagen.jpg 2560w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Karbonatfragment-mit-Sinterlagen-300x192.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Karbonatfragment-mit-Sinterlagen-1024x657.jpg 1024w, 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class=\"has-big-font-size\"><\/p>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/regelmaessige-reinigung-hat-wasserversorgung-ueber-roemischen-aquaedukt-von-divona-gesichert\/\"><strong>Regular cleaning secured water supply via the Roman aqueduct of Divona<\/strong><\/a> Calcareous deposits in the water channel were systematically removed \/ Maintenance in accordance with Roman recommendations<\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\"><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\\\/09_geowiss_divona_opus_signinum-1024x768-1.jpg&quot;,\n        &quot;id&quot;: 14351,\n        &quot;title&quot;: &quot;09_geowiss_divona_opus_signinum-1024x768&quot;,\n        &quot;width&quot;: 1024,\n        &quot;height&quot;: 768,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_divona_opus_signinum-1024x768-1.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_divona_opus_signinum-1024x768-1-300x225.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_divona_opus_signinum-1024x768-1-768x576.jpg 768w&quot;\n    },\n    &quot;caption&quot;: &quot;Masonry channel with Opus Signinum as water protection&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/der-aquaedukt-von-konstantinopel-wie-der-laengste-wasserkanal-der-antike-gewartet-wurde\/\"><strong>The aqueduct of Constantinople: How the longest water channel of antiquity was maintained<\/strong><\/a> Double water channels possibly served to maintain the facility during ongoing operation <\/li>\n<\/ul>\n\n\n\n<p class=\"has-big-font-size\"><\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\">\n<p class=\"has-big-font-size\"><\/p>\n\n\n<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\\\/09_geowiss_valens_aquaedukt_kursunlugerme-bruecke.jpg&quot;,\n        &quot;id&quot;: 14357,\n        &quot;title&quot;: &quot;09_geowiss_valens_aquaedukt_kursunlugerme-bruecke&quot;,\n        &quot;width&quot;: 1477,\n        &quot;height&quot;: 961,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_valens_aquaedukt_kursunlugerme-bruecke.jpg 1477w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_valens_aquaedukt_kursunlugerme-bruecke-300x195.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_valens_aquaedukt_kursunlugerme-bruecke-1024x666.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_valens_aquaedukt_kursunlugerme-bruecke-768x500.jpg 768w&quot;\n    },\n    &quot;caption&quot;: &quot;Two-story Kur\\u015funlugerme Bridge of the aqueduct of Constantinople&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:44.45%\">\n<ul class=\"wp-block-list\">\n<li><a href=\"https:\/\/presse.uni-mainz.de\/materialverlust-bei-der-produktion-von-marmorplatten-war-in-der-roemischen-kaiserzeit-womoeglich-niedriger-als-heute\/\"><strong>Material loss in the production of marble slabs was possibly lower in the Roman Imperial period than today<\/strong><\/a> Analysis of wall cladding from the 2nd century provides new insights into marble extraction and processing <\/li>\n<\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:22.22%\"><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\\\/09_geowiss_ephesos_marmorplatten-scaled.jpg&quot;,\n        &quot;id&quot;: 14360,\n        &quot;title&quot;: &quot;09_geowiss_ephesos_marmorplatten&quot;,\n        &quot;width&quot;: 1920,\n        &quot;height&quot;: 2560,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_ephesos_marmorplatten-scaled.jpg 1920w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_ephesos_marmorplatten-225x300.jpg 225w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_ephesos_marmorplatten-768x1024.jpg 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_ephesos_marmorplatten-1152x1536.jpg 1152w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/09_geowiss_ephesos_marmorplatten-1536x2048.jpg 1536w&quot;\n    },\n    &quot;caption&quot;: &quot;A pair of marble slabs in typical, mirror-reversed arrangement&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image><\/div>\n<\/div>\n<\/div><\/div>\n<\/jgu-base-section><jgu-base-section react-props=\"{&quot;color&quot;:&quot;light&quot;,&quot;metadata&quot;:{&quot;name&quot;:&quot;Team&quot;},&quot;align&quot;:&quot;wide&quot;,&quot;padding&quot;:&quot;medium&quot;}\">\n<div class=\"jgu-bgsection bg bg-light \"><div class=\"content padding-medium\"><div\n\tclass=\"jgu-anchorpoint\"\n\tid=\"team\"\n\tdata-label=\"Team\"\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;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;Team&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    &quot;color&quot;: &quot;red&quot;\n}\"><\/jgu-base-heading>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 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-idm-person react-props=\"{\n    &quot;id&quot;: &quot;674&quot;,\n    &quot;organizationId&quot;: 974,\n    &quot;roleId&quot;: 13,\n    &quot;name&quot;: &quot;&quot;,\n    &quot;link&quot;: &quot;idm&quot;,\n    &quot;skipDetails&quot;: [],\n    &quot;align&quot;: &quot;left&quot;,\n    &quot;color&quot;: &quot;default&quot;,\n    &quot;mode&quot;: &quot;edit&quot;,\n    &quot;linkType&quot;: &quot;idm&quot;\n}\">\n        \n<\/jgu-base-idm-person>\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;Research profile&quot;,\n    &quot;link&quot;: {\n        &quot;url&quot;: &quot;https:\\\/\\\/www.geosciences.uni-mainz.de\\\/univ-prof-dr-cees-passchier\\\/&quot;,\n        &quot;linkTarget&quot;: &quot;&quot;,\n        &quot;rel&quot;: &quot;&quot;,\n        &quot;opensInNewTab&quot;: true\n    },\n    &quot;align&quot;: &quot;left&quot;,\n    &quot;styling&quot;: &quot;primary&quot;,\n    &quot;icon&quot;: &quot;arrow-right-solid&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%\"><jgu-base-contactcard react-props=\"{\n    &quot;name&quot;: &quot;S\\u00fcrmelihindi, G\\u00fcl&quot;,\n    &quot;avatar&quot;: {\n        &quot;id&quot;: null,\n        &quot;url&quot;: null,\n        &quot;credit&quot;: &quot;&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;Research Assistant&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;university-solid&quot;,\n    &quot;title&quot;: &quot;Geoarchaeology&quot;,\n    &quot;uuid&quot;: &quot;1773144984525&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 react-props=\"{\n    &quot;uuid&quot;: &quot;1773738866122&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;title&quot;: &quot;&quot;,\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>\n\n<\/jgu-base-contactcard>\n\n\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/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-idm-person react-props=\"{\n    &quot;id&quot;: &quot;&quot;,\n    &quot;name&quot;: &quot;&quot;,\n    &quot;link&quot;: &quot;idm&quot;,\n    &quot;organizationId&quot;: 0,\n    &quot;roleId&quot;: 0,\n    &quot;skipDetails&quot;: [],\n    &quot;align&quot;: &quot;left&quot;,\n    &quot;color&quot;: &quot;default&quot;,\n    &quot;mode&quot;: &quot;edit&quot;,\n    &quot;linkType&quot;: &quot;idm&quot;\n}\">\n        \n<\/jgu-base-idm-person>\n<\/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-idm-person react-props=\"{\n    &quot;id&quot;: &quot;&quot;,\n    &quot;name&quot;: &quot;&quot;,\n    &quot;link&quot;: &quot;idm&quot;,\n    &quot;organizationId&quot;: 0,\n    &quot;roleId&quot;: 0,\n    &quot;skipDetails&quot;: [],\n    &quot;align&quot;: &quot;left&quot;,\n    &quot;color&quot;: &quot;default&quot;,\n    &quot;mode&quot;: &quot;edit&quot;,\n    &quot;linkType&quot;: &quot;idm&quot;\n}\">\n        \n<\/jgu-base-idm-person>\n<\/div>\n<\/div>\n<\/div><\/div>\n<\/jgu-base-section><jgu-base-section react-props=\"{&quot;color&quot;:&quot;white-dark-text&quot;,&quot;metadata&quot;:{&quot;name&quot;:&quot;Labore&quot;},&quot;align&quot;:&quot;wide&quot;,&quot;padding&quot;:&quot;medium&quot;}\">\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><div\n\tclass=\"jgu-anchorpoint\"\n\tid=\"laboratories\"\n\tdata-label=\"Laboratories\"\n\tdata-hide-in-nav=\"false\"\n\ttabindex=\"0\"\n\tdata-initial-scroll=\"true\"\n><\/div>\n\n\n\n<div class=\"wp-block-group is-layout-constrained wp-block-group-is-layout-constrained\"><\/div>\n\n\n<jgu-base-heading react-props=\"{\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;Laboratories&lt;br&gt;&quot;,\n    &quot;className&quot;: &quot;alignwide&quot;,\n    &quot;textAlign&quot;: &quot;left&quot;,\n    &quot;anchor&quot;: &quot;&quot;,\n    &quot;index&quot;: &quot;&quot;,\n    &quot;color&quot;: &quot;red&quot;\n}\"><\/jgu-base-heading>\n\n\n\n<p class=\"has-big-font-size\">We use other laboratories for our research work<\/p>\n<\/div><\/div>\n<\/jgu-base-section><jgu-base-section react-props=\"{&quot;color&quot;:&quot;white-dark-text&quot;,&quot;metadata&quot;:{&quot;name&quot;:&quot;Lehre&quot;},&quot;align&quot;:&quot;wide&quot;,&quot;padding&quot;:&quot;medium&quot;}\">\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><div\n\tclass=\"jgu-anchorpoint\"\n\tid=\"teaching\"\n\tdata-label=\"Teaching\"\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;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;Teaching&quot;,\n    &quot;className&quot;: &quot;alignwide&quot;,\n    &quot;textAlign&quot;: &quot;left&quot;,\n    &quot;anchor&quot;: &quot;&quot;,\n    &quot;index&quot;: &quot;&quot;,\n    &quot;color&quot;: &quot;red&quot;\n}\"><\/jgu-base-heading>\n\n\n<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\\\/Microtectonics-course-JGU.png&quot;,\n        &quot;id&quot;: 14309,\n        &quot;title&quot;: &quot;Microtectonics course JGU&quot;,\n        &quot;width&quot;: 2244,\n        &quot;height&quot;: 945,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU.png 2244w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-300x126.png 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-1024x431.png 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-768x323.png 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-1536x647.png 1536w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-2048x862.png 2048w&quot;\n    },\n    &quot;caption&quot;: &quot;Microtectonics Masterclass at JGU Mainz&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image>\n\n\n<p class=\"has-big-font-size\"><strong>Next class in Mainz will be from 17.2.2026 to 26.2.2026<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size\"><em>It is possible to participate in only Part I (17th-21st of February) or Part II (23rd-26th of February) of the Microtectonics Masterclass, but we recommend joining both since they are complimentary. We invite participants external to the University of Mainz to join us for the classes, for a fee detailed below.  <\/em><\/p>\n\n\n\n<p class=\"has-big-font-size\"><strong>If you want to register, or have any questions, please send an <a href=\"mailto:hawemann@uni-mainz.de\">e-mail<\/a> to Friedrich Hawemann.<\/strong><\/p>\n\n\n\n<p class=\"has-big-font-size\">We offer two linked <strong>practical Masterclasses in Microtectonics<\/strong> at the University of Mainz, Germany. These courses should interest students, postdocs and professionals who wish to learn about the deformation of rocks on the microscopic scale. <\/p>\n\n\n\n<p class=\"has-big-font-size\"><\/p>\n\n\n<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;Masterclass Microtectonics&quot;,\n    &quot;slug&quot;: &quot;masterclass-microtectonics&quot;,\n    &quot;metadata&quot;: {\n        &quot;name&quot;: &quot;MSc class&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-9d6595d7 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\">Masterclass Microtectonics<\/p>\n\n\n\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n<p class=\"has-big-font-size\"><strong>Part I:<\/strong> Delivered by <strong>Prof. Virginia Toy<\/strong> and <strong>Dr. Friedrich Hawemann<\/strong>, which is entitled &#8220;Fault Rocks and Fault Mechanisms Revisited&#8221; will focus on how fault zone processes can be inferred from their textural record. The class will examine the set of thin sections and samples of fault rocks (mylonites, cataclasites, pseudotachylytes) from the Outer Hebrides Fault Zone (Scotland) that inspired Sibson (1977) to develop his widely-cited classification of fault rocks, and from New Zealand&#8217;s Alpine Fault Zone where he next applied this classification. Additionally, a set of exercises will examine microstructural datasets from both Outer Hebrides and Alpine Fault Zone samples acquired using advanced analytical tools, including SEM (EBSD, BSE-imaging), TEM, and synchrotron-CT. These exercises will demonstrate how to quantify the 2D and 3D arrangement and shapes of fault rock grains and particles, their textures, their crystallographic orientations, and the nature of porosity. The implications for fault rheology will be explored.    <\/p>\n\n\n\n<p class=\"has-big-font-size\"><strong>Part II:<\/strong> Delivered by <strong>Prof. Cees Passchier<\/strong>, teaches how deformation mechanisms can be inferred from the microstructures visible in thin sections. It is based on the book &#8220;Microtectonics&#8221; by Passchier and Trouw (2005), and the superb Microtectonics Collection of 300 selected thin sections that are the source of figures in that book will be examined during the course. The main topics, which are treated through an alternation of lectures and microscopy practicals, are: Principles of microtectonic analysis, overprinting relations, deformation phases and tectonic phases, flow and deformation, intracrystalline deformation, foliations and lineations, shear zones, veins and fringes, porphyroblasts, metamorphic reaction rims.  <\/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\\\/Microtectonics-course-JGU-2.png&quot;,\n        &quot;id&quot;: 14375,\n        &quot;title&quot;: &quot;Microtectonics course JGU-2&quot;,\n        &quot;width&quot;: 2244,\n        &quot;height&quot;: 945,\n        &quot;srcset&quot;: 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2048w&quot;\n    },\n    &quot;caption&quot;: &quot;Deformation structure&quot;,\n    &quot;align&quot;: &quot;&quot;,\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-\">\n    \n<\/jgu-base-image>\n\n\n<div style=\"height:164px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<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\\\/Microtectonics-course-JGU-3.png&quot;,\n        &quot;id&quot;: 14372,\n        &quot;title&quot;: &quot;Microtectonics course JGU-3&quot;,\n        &quot;width&quot;: 2244,\n        &quot;height&quot;: 945,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3.png 2244w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3-300x126.png 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3-1024x431.png 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3-768x323.png 768w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3-1536x647.png 1536w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Microtectonics-course-JGU-3-2048x862.png 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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<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\\\/Cees-Publikationen.jpg&quot;,\n        &quot;id&quot;: 14408,\n        &quot;title&quot;: &quot;Cees Publikationen&quot;,\n        &quot;width&quot;: 1319,\n        &quot;height&quot;: 546,\n        &quot;srcset&quot;: &quot;https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Cees-Publikationen.jpg 1319w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Cees-Publikationen-300x124.jpg 300w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Cees-Publikationen-1024x424.jpg 1024w, https:\\\/\\\/cms.zdv.uni-mainz.de\\\/fb09-geowissenschaften\\\/wp-content\\\/uploads\\\/sites\\\/789\\\/2026\\\/03\\\/Cees-Publikationen-768x318.jpg 768w&quot;\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    \n<\/jgu-base-image>\n\n\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n<p class=\"has-big-font-size\"><\/p>\n\n\n\n\n<h3>2026<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Surmelihindi, G., Passchier, C., Trumper, M., et al. (2026). Seeing Roman life through water: Exploring Pompeii\u2019s public baths via carbonate deposits. <i>PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA<\/i>, <i>123<\/i>(3). <a href=\"https:\/\/doi.org\/10.1073\/pnas.2517276122\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001720726000001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2025<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Konopasek, J., Oyhantcabal, P., Passchier, C. W., et al. (2025). Pre- and syn-orogenic sedimentation and volcanic activity in the internal domain of the southern Kaoko-Dom Feliciano-Gariep orogenic system. <i>JOURNAL OF THE GEOLOGICAL SOCIETY<\/i>, <i>182<\/i>(5). <a href=\"https:\/\/doi.org\/10.1144\/jgs2025-070\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001528485000001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Surmelihindi, G., Passchier, C., Wilson, A., Spotl, C. (2025). The Roman Water Management of Arles as Read in Aqueduct Carbonate Archives. <i>GEOARCHAEOLOGY-AN INTERNATIONAL JOURNAL<\/i>, <i>40<\/i>(4). <a href=\"https:\/\/doi.org\/10.1002\/gea.70020\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001559501500004&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Wassenaar, T. M., Groschopf, N., et al. (2025). Subfossil Fracture-Related Euendolithic Micro-burrows in Marble and Limestone. <i>GEOMICROBIOLOGY JOURNAL<\/i>, <i>42<\/i>(5), 390-405. <a href=\"https:\/\/doi.org\/10.1080\/01490451.2025.2467417\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001433546600001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2024<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Claude, C., Vidal, L., Passchier, C., et al. (2024). High resolution paleo-hydrological record from carbonate deposits in the Roman aqueduct of Traconnade (Aix-en-Provence, SE France). <i>Chemical Geology<\/i>, <i>670<\/i>, 122423-122423. <a href=\"https:\/\/doi.org\/10.1016\/j.chemgeo.2024.122423\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Suermelihindi, G., Viollet, P.-L., et al. (2024). Operation and decline of the Barbegal mill complex, the largest industrial complex of antiquity. <i>GEOARCHAEOLOGY-AN INTERNATIONAL JOURNAL<\/i>, <i>39<\/i>(6), 594-608. <a href=\"https:\/\/doi.org\/10.1002\/gea.22016\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001257401400001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Angelakis, A. N., Baba, A., Valipour, M., et al. (2024). Water Dams: From Ancient to Present Times and into the Future. <i>WATER<\/i>, <i>16<\/i>(13). <a href=\"https:\/\/doi.org\/10.3390\/w16131889\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001269731300001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Correction to \u201cWrit in water\u2014Unwritten histories obtained from carbonate deposits in ancient water systems\u201d. (2024). <i>Geoarchaeology<\/i>, <i>39<\/i>(3), 351-351. <a href=\"https:\/\/doi.org\/10.1002\/gea.22000\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">S\u00fcrmelihindi, G., Passchier, C. (2024). Writ in water\u2014Unwritten histories obtained from carbonate deposits in ancient water systems. <i>Geoarchaeology<\/i>, <i>39<\/i>(1), 63-88. <a href=\"https:\/\/doi.org\/10.1002\/gea.21980\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2023<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Angelakis, A. N., Passchier, C. W., Valipour, M., et al. (2023). Evolution of Tunneling Hydro-Technology: From Ancient Times to Present and Future. <i>HYDROLOGY<\/i>, <i>10<\/i>(9). <a href=\"https:\/\/doi.org\/10.3390\/hydrology10090190\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:001073777800001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Angelakis, A. N., Capodaglio, A. G., Passchier, C. W., et al. (2023). Sustainability of Water, Sanitation, and Hygiene: From Prehistoric Times to the Present Times and the Future. <i>WATER<\/i>, <i>15<\/i>(8). <a href=\"https:\/\/doi.org\/10.3390\/w15081614\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000983108800001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Rigal, D., Passchier, C. W., S\u00fcrmelihindi, G. (2023). Origines, d\u00e9veloppement et preuves du nettoyage des concr\u00e9tions calcaires durant le fonctionnement de l\u2019aqueduc gallo-romain de Divona-Cahors (Lot). <i>Arch\u00e9ologie, soci\u00e9t\u00e9 et environnement<\/i>, <i>1<\/i>(1). <a href=\"https:\/\/doi.org\/10.21494\/iste.op.2023.0944\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2022<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Ghanem, H., Jarrar, G. H., McAleer, R. J., et al. (2022). Drowned in granite &#8211; retrieving the tectono-metamorphic history of the Janub metamorphic complex, the northernmost part of the Arabian-Nubian Shield. <i>Precambrian Research<\/i>, <i>383<\/i>, 106903-106903. <a href=\"https:\/\/doi.org\/10.1016\/j.precamres.2022.106903\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2021<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Suermelihindi, G., Passchier, C., Crow, J., et al. (2021). Carbonates from the ancient world\u2019s longest aqueduct: A testament of Byzantine water management. <i>GEOARCHAEOLOGY-AN INTERNATIONAL JOURNAL<\/i>, <i>36<\/i>(4), 643-659. <a href=\"https:\/\/doi.org\/10.1002\/gea.21853\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000647547400001&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Wex, S., Ilhan, S., et al. (2021). Analysis of Cipollino Verde marble wall decoration in Ephesos, Turkey, using geological reconstruction. <i>Journal of Archaeological Science: Reports<\/i>, <i>37<\/i>, 102992-102992. <a href=\"https:\/\/doi.org\/10.1016\/j.jasrep.2021.102992\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C., Suermelihindi, G., Boyer, D., et al. (2021). The aqueduct of Gerasa &#8211; Intra-annual palaeoenvironmental data from Roman Jordan using carbonate deposits. <i>PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY<\/i>, <i>562<\/i>. <a href=\"https:\/\/doi.org\/10.1016\/j.palaeo.2020.110089\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000604584600024&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2020<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W., Bourgeois, M., Viollet, P.-L., et al. (2020). Reconstructing the hydraulics of the world\u2019s first industrial complex, the second century CE Barbegal watermills, France. <i>Scientific Reports<\/i>, <i>10<\/i>(1). <a href=\"https:\/\/doi.org\/10.1038\/s41598-020-74900-5\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2019<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">S\u00fcrmelihindi, G., Passchier, C. W., Leveau, P., et al. (2019). Barbegal: carbonate imprints give a voice to the first industrial complex of Europe. <i>Journal of Archaeological Science: Reports<\/i>, <i>24<\/i>, 1041-1058. <a href=\"https:\/\/doi.org\/10.1016\/j.jasrep.2019.02.031\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2018<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Nascimento, D. B., Ribeiro, A., Trouw, R. A. J., et al. (2018). Reply to discussion by Hoffman and Halverson (2018) on the article: \u201cDepositional ages and provenance of the Neoproterozoic Damara Supergroup: (northwest Namibia): Implications for the Angola-Congo and Kalahari cratons connection\u201d by Nascimento et al. (2017), Gondwana Research 52, 153\u2013171. <i>Gondwana Research<\/i>, <i>58<\/i>, 239-240. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2018.02.004\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">S\u00fcrmelihindi, G., Leveau, P., Sp\u00f6tl, C., et al. (2018). The second century CE Roman watermills of Barbegal : unraveling the enigma of one of the oldest industrial complexes. <i>Science advances<\/i>, <i>4<\/i>(9), eaar3620. <a href=\"http:\/\/dx.doi.org\/10.1126\/sciadv.aar3620\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2017<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Nascimento, D. B., Schmitt, R. S., Ribeiro, A., et al. (2017). Depositional ages and provenance of the Neoproterozoic Damara Supergroup (northwest Namibia): Implications for the Angola-Congo and Kalahari cratons connection. <i>Gondwana Research<\/i>, <i>52<\/i>, 153-171. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2017.09.006\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Salomon, E., Passchier, C., Koehn, D. (2017). Asymmetric continental deformation during South Atlantic rifting along southern Brazil and Namibia. <i>Gondwana Research<\/i>, <i>51<\/i>, 170-176. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2017.08.001\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Jarrar, G. H., Stern, R. J., Theye, T., et al. (2017). Neoproterozoic Rosetta Gabbro from northernmost Arabian\u2013Nubian Shield, south Jordan: Geochemistry and petrogenesis. <i>Lithos<\/i>, <i>284-285<\/i>, 545-559. <a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2017.05.008\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Meyer, S. E., Kaus, B. J. P., Passchier, C. (2017). Development of branching brittle and ductile shear zones: A numerical study. <i>GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS<\/i>, <i>18<\/i>(6), 2054-2075. <a href=\"https:\/\/doi.org\/10.1002\/2016GC006793\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000405585000003&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Meyer, S. E., Passchier, C., Jarrar, G. H., et al. (2017). Mimicking shear zones: An example from Wadi Filk, Jordan. <i>Journal of Structural Geology<\/i>, <i>98<\/i>, 83-94. <a href=\"https:\/\/doi.org\/10.1016\/j.jsg.2017.03.010\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Platt, J. P. (2017). Shear zone junctions: Of zippers and freeways. <i>Journal of Structural Geology<\/i>, <i>95<\/i>, 188-202. <a href=\"https:\/\/doi.org\/10.1016\/j.jsg.2016.10.010\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2016<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C., Suermelihindi, G., Spoetl, C., et al. (2016). Carbonate deposits from the ancient aqueduct of Beziers, France &#8211; A high-resolution palaeoenvironmental archive for the Roman Empire. <i>PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY<\/i>, <i>461<\/i>, 328-340. <a href=\"https:\/\/doi.org\/10.1016\/j.palaeo.2016.08.022\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000385599900026&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C., Trouw, R., da Silva Schmitt, R. (2016). How to make a transverse triple junction\u2014New evidence for the assemblage of Gondwana along the Kaoko-Damara belts, Namibia. <i>Geology<\/i>, <i>44<\/i>(10), 843-846. <a href=\"https:\/\/doi.org\/10.1130\/g38015.1\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Platt, J. P., Passchier, C. W. (2016). Zipper junctions: A new approach to the intersections of conjugate strike-slip faults. <i>Geology<\/i>, <i>44<\/i>(10), 795-798. <a href=\"https:\/\/doi.org\/10.1130\/g38058.1\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Link, K., Sachau, T., et al. (2016). The Rwenzori Mountains, a Palaeoproterozoic crustal shear belt crossing the Albertine rift system. <i>International Journal of Earth Sciences<\/i>, <i>105<\/i>(6), 1693-1705. <a href=\"https:\/\/doi.org\/10.1007\/s00531-015-1167-1\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Nascimento, D. B., Ribeiro, A., Trouw, R. A. J., et al. (2016). Stratigraphy of the Neoproterozoic Damara Sequence in northwest Namibia: Slope to basin sub-marine mass-transport deposits and olistolith fields. <i>Precambrian Research<\/i>, <i>278<\/i>, 108-125. <a href=\"https:\/\/doi.org\/10.1016\/j.precamres.2016.03.005\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Wenz, S., Scholz, D., Suermelihindi, G., et al. (2016). &lt;SUP&gt;230&lt;\/SUP&gt;Th\/U-dating of carbonate deposits from ancient aqueducts. <i>QUATERNARY GEOCHRONOLOGY<\/i>, <i>32<\/i>, 40-52. <a href=\"https:\/\/doi.org\/10.1016\/j.quageo.2015.12.001\" title=\"Bibliographical information\">DOI<\/a> <a href=\"https:\/\/www.webofscience.com\/api\/gateway?GWVersion=2&#038;SrcApp=fis-test-1&#038;SrcAuth=WosAPI&#038;KeyUT=WOS:000369457200005&#038;DestLinkType=FullRecord&#038;DestApp=WOS_CPL\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., S\u00fcrmelihindi, G., Sp\u00f6tl, C. (2016). A high-resolution palaeoenvironmental record from carbonate deposits in the Roman aqueduct of Patara, SW Turkey, from the time of Nero. <i>Scientific reports<\/i>, <i>6<\/i>, Art. 28704. <a href=\"http:\/\/dx.doi.org\/10.1038\/srep28704\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Salomon, E., Koehn, D., Passchier, C. W., et al. (2016). Deformation and fluid flow in the Huab Basin and Etendeka Plateau, NW Namibia. <i>Journal of structural geology<\/i>, <i>88<\/i>, Seiten: 46-62. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2016.05.001\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2015<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Ghani, I., Koehn, D., Toussaint, R., Passchier, C. W. (2015). Dynamics of hydrofracturing and permeability evolution in layered reservoirs. <i>Frontiers in Physics<\/i>, <i>3<\/i>. <a href=\"https:\/\/doi.org\/10.3389\/fphy.2015.00067\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (2015). Preuves du nettoyage des concr\u00e9tions calcaires de l\u2019aqueduc antique de Divona-Cahors. <i>Aquitania supplement<\/i>, <i>33<\/i>, 233-241.<\/div>\n  <div class=\"csl-entry\">Salomon, E., Koehn, D., Passchier, C. W. (2015). Brittle reactivation of ductile shear zones in NW Namibia in relation to South Atlantic rifting. <i>Tectonics<\/i>, <i>34<\/i>(1), Seiten: 70-85. <a href=\"http:\/\/dx.doi.org\/10.1002\/2014TC003728\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Salomon, E., Koehn, D., Passchier, C. W., et al. (2015). Contrasting stress fields on correlating margins of the South Atlantic. <i>Gondwana research<\/i>, <i>28<\/i>(3), Seiten: 1152-1167. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.gr.2014.09.006\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2014<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Meyer, S. E., Passchier, C., Abu\u2010Alam, T., and St\u00fcwe, K. (2014). A strike\u2010slip core complex from the Najd fault system, Arabian shield. <i>Terra Nova<\/i>, <i>26<\/i>(5), 387-394. <a href=\"https:\/\/doi.org\/10.1111\/ter.12111\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Wex, S., Passchier, C. W., de Kemp, E. A., and \u0130lhan, S. (2014). 3D visualization of sheath folds in Ancient Roman marble wall coverings from Ephesos, Turkey. <i>Journal of Structural Geology<\/i>, <i>67<\/i>, 129-139. <a href=\"https:\/\/doi.org\/10.1016\/j.jsg.2014.07.005\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (2014). Exhumation of Mid-Crustal Rocks in the Arabian-Nubian Shield. The Baladaya Complex of Saudi Arabia. <i>Journal of Petrology<\/i>, <i>55<\/i>, 1941-1964.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>2013<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Arslan, A., G\u00fcng\u00f6r, T., Erdogan, B., Passchier, C. W. (2013). Tectonic transport directions of the Lycian nappes in Southwest Turkey constrained by kinematic indicators. <i>Journal of asian earth sciences<\/i>, <i>64<\/i>, Seiten: 198-209. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jseaes.2012.12.016\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">De Feo, G., Angelakis, A. N., Antoniou, G. P., et al. (2013). Historical and technical notes on aqueducts from prehistoric to medieval times. <i>Water<\/i>, <i>5<\/i>(4), Seiten: 1996-2025. <a href=\"http:\/\/dx.doi.org\/10.3390\/w5041996\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Druguet, E., Passchier, C. W., Pennacchioni, G., Carreras, J. (2013). Geoethical education : a critical issue for geoconservation. <i>Episodes<\/i>, <i>36<\/i>(1), Seiten: 11-18.<\/div>\n  <div class=\"csl-entry\">Ghani, I., Koehn, D., Toussaint, R., Passchier, C. W. (2013). Dynamic development of hydrofracture. <i>Pure and applied geophysics<\/i>, <i>170<\/i>(11), Seiten: 1685-1703. <a href=\"http:\/\/dx.doi.org\/10.1007\/s00024-012-0637-7\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Jarrar, G. H., Theye, T., Yaseen, N., et al. (2013). Geochemistry and P-T-t evolution of the Abu-Barqa Metamorphic Suite, SW Jordan, and implications for the tectonics of the northern Arabian-Nubian Shield. <i>Precambrian research<\/i>, <i>239<\/i>, Seiten: 56-78. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.precamres.2013.08.003\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., S\u00fcrmelihindi, G., Baykan, O. N., et al. (2013). Environmental and depositional controls on laminated freshwater carbonates : an example from the Roman aqueduct of Patara, Turkey. <i>Palaeogeography, palaeoclimatology, palaeoecology<\/i>, <i>386<\/i>, Seiten: 321-335. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.palaeo.2013.06.002\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Wiplinger, G., G\u00fcng\u00f6r, T., et al. (2013). Normal fault displacement dislocating a Roman aqueduct of Ephesos, Eastern Turkey. <i>Terra nova<\/i>, <i>25<\/i>(4), Seiten: 292-297. <a href=\"http:\/\/dx.doi.org\/10.1111\/ter.12035\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Sachau, T., Koehn, D., Passchier, C. W. (2013). Mountain-building under extension. <i>American journal of science<\/i>, <i>313<\/i>(4), Seiten: 326-344. <a href=\"http:\/\/dx.doi.org\/10.2475\/04.2013.03\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">S\u00fcrmelihindi, G., Passchier, C. W., Sp\u00f6tl, C., et al. (2013). Laminated carbonate deposits in roman aqueducts : origin, processes and implications. <i>Sedimentology<\/i>, <i>60<\/i>(4), Seiten: 961-982. <a href=\"http:\/\/dx.doi.org\/10.1111\/sed.12000\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2012<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W., Myers, J. S., Kr\u00f6ner, A. (2012). <i>Field Geology of High-Grade Gneiss Terrains<\/i>. Springer Science &amp; Business Media.<\/div>\n  <div class=\"csl-entry\">Schmitt, R. S., Trouw, R. A. J., Passchier, C. W., et al. (2012). 530Ma syntectonic syenites and granites in NW Namibia \u2014 Their relation with collision along the junction of the Damara and Kaoko belts. <i>Gondwana Research<\/i>, <i>21<\/i>(2-3), 362-377. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2011.08.006\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Arslan, A., Koehn, D., Passchier, C. W., Sachau, T. (2012). The transition from single layer to foliation boudinage : a dynamic modelling approach. <i>Journal of structural geology<\/i>, <i>42<\/i>, Seiten: 118-126. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2012.06.005\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Ebner, M., Renard, F., et al. (2012). Modelling of stylolite geometries and stress scaling. <i>Earth and planetary science letters<\/i>, <i>341\/344<\/i>, Seiten: 104-113. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.epsl.2012.04.046\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Salomon, E., Koehn, D., Passchier, C. W., et al. (2012). Shear zone reactivation during South Atlantic rifting in NW Namibia. <i>Geophysical research abstracts<\/i>, <i>14<\/i>, Seite: 11071.<\/div>\n  <div class=\"csl-entry\">Schmitt, R. S., Rouw, R. A. J., Passchier, C. W., et al. (2012). 530 Ma syntectonic syenites and granites in NW Namibia : their relation with collision along the junction of the Damara and Kaoko belts. <i>Gondwana research<\/i>, <i>21<\/i>(2\/3), Seiten: 362-377. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.gr.2011.08.006\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2011<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Oyhant\u00e7abal, P., Siegesmund, S., Wemmer, K., and Passchier, C. W. (2011). The transpressional connection between Dom Feliciano and Kaoko Belts at 580 550\u00a0Ma. <i>International journal of earth sciences<\/i>, <i>100<\/i>, Seiten: 379-390. <a href=\"http:\/\/dx.doi.org\/10.1007\/s00531-010-0577-3\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2010<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Koehn, D., Lindenfeld, M., R\u00fcmpker, G., et al. (2010). Active transsection faults in rift transfer zones : evidence for complex stress fields and implications for crustal fragmentation processes in the western branch of the East African Rift. <i>International journal of earth sciences<\/i>, <i>99<\/i>(7), Seiten: 1633-1642. <a href=\"http:\/\/dx.doi.org\/10.1007\/s00531-010-0525-2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Exner, U. (2010). Digital mapping in structural geology examples from Namibia and Greece. <i>Journal of the geological society of India<\/i>, <i>75<\/i>, Seiten: 32-42.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>2009<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Trouw, R. A. J., Passchier, C. W., and Wiersma, D. J. (2009). <i>Atlas of Mylonites &#8211; and related microstructures<\/i>. Springer Science &amp; Business Media.<\/div>\n  <div class=\"csl-entry\">Maeder, X., Passchier, C. W., and Koehn, D. (2009). Modelling of segment structures : boudins, bone-boudins, mullions and related single- and multiphase deformation features. <i>Journal of structural geology<\/i>, <i>31<\/i>(8), Seiten: 817-830. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2009.05.013\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Robyr, M., Carlson, W. D., Passchier, C. W., and Vonlanthen, P. (2009). Microstructural, chemical and textural records during growth of snowball garnet. <i>Journal of metamorphic geology<\/i>, <i>27<\/i>(6), Seiten: 423-437. <a href=\"http:\/\/dx.doi.org\/10.1111\/j.1525-1314.2009.00824.x\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2008<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Arslan, A., Passchier, C. W., Koehn, D. (2008). Foliation boudinage. <i>Journal of structural geology<\/i>, <i>30<\/i>(3), Seiten: 291-309. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2007.11.004\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Coelho, S., Passchier, C. W. (2008). Mohr-cyclides, a 3D representation of geological tensors : the examples of stress and flow. <i>Journal of structural geology<\/i>, <i>30<\/i>(5), Seiten: 580-601. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2008.01.003\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Gray, D. R., Foster, D. A., Meert, J. G., et al. (2008). A Damara orogen perspective on the assembly of southwestern Gondwana. <i>Special publications : the Geological Society, London<\/i>, <i>294<\/i>(1), Seiten: 257-278. <a href=\"http:\/\/dx.doi.org\/10.1144\/SP294.14\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Iacopini, D., Carosi, R., Montomoli, C., Passchier, C. W. (2008). Strain analysis and vorticity of flow in the Northern Sardinian Variscan Belt : recognition of a partitioned oblique deformation event. <i>Tectonophysics<\/i>, <i>446<\/i>(1\/4), Seiten: 77-96. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.tecto.2007.10.002\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C., Heesakkers, V., Coelho, S. (2008). Two mechanisms for forming flanking folds. <i>Journal of the Virtual Explorer<\/i>, <i>30<\/i>. <a href=\"https:\/\/doi.org\/10.3809\/jvirtex.2009.00209\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Schmitt, R. S., Trouw, R. A. J., Van Schmus, W. R., Passchier, C. W. (2008). Cambrian orogeny in the Ribeira Belt (SE Brazil) and correlations within West Gondwana : ties that bind underwater. In R. J. Pankhurst (ed.), <i>West Gondwana : pre-cenozoic correlations across the South Atlantic region<\/i> (pp. Seiten: 279-296). London:Geological Soc.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>2007<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Iacopini, D., Passchier, C. W., Koehn, D., Carosi, R. (2007). Fabric attractors in general triclinic flow systems and their application to high strain shear zones : a dynamical system approach. <i>Journal of structural geology<\/i>, <i>29<\/i>(2), Seiten: 298-317. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2006.10.002\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Renard, F., Toussaint, R., Passchier, C. W. (2007). Growth of stylolite teeth patterns depending on normal stress and finite compaction. <i>Earth and planetary science letters<\/i>, <i>257<\/i>(3\/4), Seiten: 582-595. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.epsl.2007.03.015\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Maeder, X., Passchier, C. W., Trouw, R. A. J. (2007). Flame foliation : evidence for a schistosity formed normal to the extension direction. <i>Journal of structural geology<\/i>, <i>29<\/i>(3), Seiten: 378-384. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2006.10.005\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Paciullo, F. V. P., Ribeiro, A., Trouw, R. A. J., Passchier, C. W. (2007). Facies and facies association of the siliciclastic Brak River and carbonate Gemsbok formations in the Lower Ugab River valley, Namibia, W. Africa. <i>Journal of African earth sciences<\/i>, <i>47<\/i>(3), Seiten: 121-134. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jafrearsci.2006.12.004\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Trouw, R. A. J., Goscombe, B., et al. (2007). Intrusion mechanisms in a turbidite sequence : the Voetspoor and Doros plutons in NW Namibia. <i>Journal of structural geology<\/i>, <i>29<\/i>(3), Seiten: 481-496. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2006.09.007\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Regnier, J.-L., Mezger, J. E., Passchier, C. W. (2007). Metamorphism of Precambrian-Palaeozoic schists of the Menderes core series and contact relationships with Proterozoic orthogneisses of the western Cine Massif, Anatolide belt, western Turkey. <i>Geological magazine<\/i>, <i>144<\/i>(1), Seiten: 67-104. <a href=\"http:\/\/dx.doi.org\/10.1017\/S0016756806002640\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2006<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C., Coelho, S. (2006). An outline of shear-sense analysis in high-grade rocks. <i>Gondwana Research<\/i>, <i>10<\/i>(1-2), 66-76. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2005.11.016\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Coelho, S., Passchier, C. W., Marques, F. (2006). Riedel-shear control on the development of pennant veins : field example and analogue modelling. <i>Journal of structural geology<\/i>, <i>28<\/i>(9), Seiten: 1658-1669. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2006.05.009\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Gray, D. R., Foster, D. A., Goscombe, B., et al. (2006). 40Ar\/39Ar thermochronology of the Pan-African Damara Orogen, Namibia, with implications for tectonothermal and geodynamic evolution. <i>Precambrian research<\/i>, <i>150<\/i>(1\/2), Seiten: 49-72. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.precamres.2006.07.003\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Malthe-Sorenssen, A., Passchier, C. W. (2006). The structure of reactive grain-boundaries under stress containing confined fluids. <i>Chemical geology<\/i>, <i>230<\/i>(3\/4), Seiten: 207-219. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.chemgeo.2006.02.026\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Coelho, S. (2006). An outline of shear-sense analysis in high-grade rocks. <i>Gondwana research<\/i>, <i>10<\/i>(1\/2), Seiten: 66-76. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.gr.2005.11.016\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2005<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Coelho, S., Passchier, C. W., Grasemann, B. (2005). Geometric description of flanking structures. <i>Journal of structural geology<\/i>, <i>27<\/i>(4), Seiten: 597-606. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2004.12.002\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Grasemann, B., Martel, S., Passchier, C. W. (2005). Reverse and normal drag along a fault. <i>Journal of structural geology<\/i>, <i>27<\/i>(6), Seiten: 999-1010. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2005.04.006\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Arnold, J., Passchier, C. W. (2005). Fracture and vein patterns as indicators of deformation history : a numerical study. <i>Special publications : the Geological Society, London<\/i>, <i>243<\/i>, Seiten: 11-24. <a href=\"http:\/\/dx.doi.org\/10.1144\/GSL.SP.2005.243.01.03\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Konop\u00e1sek, J., Kr\u00f6ner, S., Kitt, S. L., et al. (2005). Oblique collision and evolution of large-scale transcurrent shear zones in the Kaoko belt, NW Namibia. <i>Precambrian research<\/i>, <i>136<\/i>(2), Seiten: 139-157. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.precamres.2004.10.005\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (2005). Field relationsips, Geochemistry, zircon ages and evolution of a late Archaean to Palaeoproterozoic Lower Crustal Section in the Hengshan Terrain of Northern China. <i>Dizhi Xuebao\/Acta Geologica Sinica<\/i>, <i>79<\/i>, 605-629.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Mancktelow, N. S., Grasemann, B. (2005). Flow perturbations : a tool to study and characterize heterogeneous deformation. <i>Journal of structural geology<\/i>, <i>27<\/i>(6), Seiten: 1011-1026. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2005.01.016\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Zhang, J. S., Konop\u00e1sek, J. (2005). Geometric aspects of synkinematic granite intrusion into a ductile shear zone an example from the Yunmengshan core complex, northern China. In Bruhn,David F. (ed.), <i>High-strain zones : structure and physical properties<\/i> (pp. Seiten: 65-80). London:Geological Society.<\/div>\n  <div class=\"csl-entry\">Walte, N. P., Bons, P. D., Passchier, C. W. (2005). Deformation of melt-bearing systems insight from in situ grain-scale analogue experiments. <i>Journal of structural geology<\/i>, <i>27<\/i>(9), Seiten: 1666-1679. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2005.05.006\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2004<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Bons, P. D., Druguet, E., Hamann, I., et al. (2004). Apparent boudinage in dykes. <i>Journal of structural geology<\/i>, <i>26<\/i>(4), Seiten: 625-636. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2003.11.009\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Goscombe, B. D., Passchier, C. W., Hand, M. (2004). Boudinage classification: end-member boudin types and modified boudin structures. <i>Journal of structural geology<\/i>, <i>26<\/i>(4), Seiten: 739-763. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.jsg.2003.08.015\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Kr\u00f6ner, S., Konop\u00e1sek, J., Kr\u00f6ner, A., et al. (2004). U-Pb and Pb-Pb zircon ages for metamorphic rocks in the Kaoko Belt of Northwestern Namibia : a palaeo- to Mesoproterozoic basement reworked during the Pan-African orogeny. <i>South African journal of geology<\/i>, <i>107<\/i>(3), Seiten: 455-476. <a href=\"http:\/\/dx.doi.org\/10.2113\/107.3.455\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Mezger, J. E., Passchier, C. W., R\u00e9gnier, J.-L. (2004). Metastable staurolite-cordierite assemblage of the Boss\u00f2st dome : Late Variscan decompression and polyphase metamorphism in the Axial Zone of the central Pyrenees. <i>Comptes Rendus Geosciences<\/i>, <i>336<\/i>(9), Seiten: 827-837. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.crte.2003.12.024\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Occhipinti, S. A., Sheppard, S., Passchier, C. W., et al. (2004). Palaeoproterozoic crustal accretion and collision in the southern Capricorn Orogen: the Glenburgh Orogeny. <i>Precambrian research<\/i>, <i>128<\/i>(3\/4), Seiten: 237-255. <a href=\"http:\/\/dx.doi.org\/10.1016\/j.precamres.2003.09.002\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2003<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Goscombe, B. D., Passchier, C. W. (2003). Asymmetric boudins as shear sense indicators : an assessment from field data. <i>Journal of structural geology<\/i>, <i>25<\/i>(4), Seiten: 575-589. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(02)00045-7\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Grotenhuis, S. M. ten, Trouw, R. A. J., Passchier, C. W. (2003). Evolution of mica fish in mylonitic rocks. <i>Tectonophysics<\/i>, <i>372<\/i>(1\/2), Seiten: 1-21. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(03)00231-2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Bons, P. D., Passchier, C. W. (2003). Development of antitaxial strain fringes during non-coaxial deformation : an experimental study. <i>Journal of structural geology<\/i>, <i>25<\/i>(2), Seiten: 263-275. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(02)00022-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Mezger, J. E., Passchier, C. W. (2003). Polymetamorphism and ductile deformation of staurolite-cordierite schist of the Bossost dome : indication for Variscan extension in the Axial Zone of the central Pyrenees. <i>Geological magazine<\/i>, <i>140<\/i>(5), Seiten: 595-612. <a href=\"http:\/\/dx.doi.org\/10.1017\/S0016756803008112\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">R\u00e9gnier, J. L., Ring, U., Passchier, C. W., et al. (2003). Contrasting metamorphic evolution of metasedimentary rocks from the \u00c7ine and Selimiye nappes in the Anatolide belt, western Turkey. <i>Journal of metamorphic geology<\/i>, <i>21<\/i>(7), Seiten: 699-721. <a href=\"http:\/\/dx.doi.org\/10.1046\/j.1525-1314.2003.00473.x\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Walte, N. P., Bons, P. D., Passchier, C. W., Koehn, D. (2003). Disequilibrium melt distribution during static recrystallization. <i>Geology<\/i>, <i>31<\/i>(11), Seiten: 1009-1012. <a href=\"http:\/\/dx.doi.org\/10.1130\/G19815.1\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2002<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Elburg, M. A., Bons, P. D., Foden, J., Passchier, C. W. (2002). The origin of fibrous veins : constraints from geochemistry. <i>Special publications : the Geological Society, London<\/i>, <i>200<\/i>, Seiten: 103-118. <a href=\"http:\/\/dx.doi.org\/10.1144\/GSL.SP.2001.200.01.07\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Druguet, E. (2002). Numerical modelling of asymmetric boudinage. <i>Journal of structural geology<\/i>, <i>24<\/i>(11), Seiten: 1789-1803. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(01)00163-8\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Trouw, R. A. J., Ribeiro, A., Paciullo, F. V. P. (2002). Tectonic evolution of the southern Kaoko belt, Namibia. <i>Journal of African Earth sciences<\/i>, <i>35<\/i>(1), Seiten: 61-75. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0899-5362(02)00030-1\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Piazolo, S., Passchier, C. W. (2002). Experimental modeling of viscous inclusions in a circular high-strain shear rig : implications for the interpretation of shape fabrics and deformed enclaves. <i>Journal of geophysical research : Solid earth<\/i>, <i>107<\/i>(B10), 2242. <a href=\"http:\/\/dx.doi.org\/10.1029\/2000JB000030\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Piazolo, S., Bons, P. D., Jessell, M. W., et al. (2002). Dominance of microstructural processes and their effect on microstructural development : insights from numerical modelling of dynamic recrystallization. <i>Special publications : the Geological Society, London<\/i>, <i>200<\/i>, Seiten: 149-170. <a href=\"http:\/\/dx.doi.org\/10.1144\/GSL.SP.2001.200.01.10\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Piazolo, S., Bons, P. D., Passchier, C. W. (2002). The influence of matrix rheology and vorticity on fabric development of populations of rigid objects during plane strain deformation. <i>Tectonophysics<\/i>, <i>351<\/i>(4), Seiten: 315-329. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(02)00220-2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Piazolo, S., Passchier, C. W. (2002). Controls on lineation development in low to medium grade shear zones : a study from the Cap de Creus peninsula, NE Spain. <i>Journal of structural geology<\/i>, <i>24<\/i>(1), Seiten: 25-44. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(01)00045-1\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">ten Grotenhuis, S. M., Passchier, C. W., Bons, P. D. (2002). The influence of strain localisation on the rotation behaviour of rigid objects in experimental shear zones. <i>Journal of tructural geology<\/i>, <i>24<\/i>(3), Seiten: 485-499. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(01)00072-4\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">ten Grotenhuis, S. M., Piazolo, S., Pakula, T., et al. (2002). Are polymers suitable rock analogs?. <i>Tectonophysics<\/i>, <i>350<\/i>(1), Seiten: 35-47. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(02)00080-X\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>2001<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Gessner, K., Piazolo, S., G\u00fcng\u00f6r, T., et al. (2001). Tectonic significance of deformation patterns in granitoid rocks of the Menderes nappes, Anatolide belt, southwest Turkey. <i>International journal of earth sciences<\/i>, <i>89<\/i>(4), Seiten: 766-780. <a href=\"http:\/\/dx.doi.org\/10.1007\/s005310000106\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Gessner, K., Ring, U., Johnson, C., et al. (2001). An active bivergent rolling-hinge detachment system : central Menderes metamorphic core complex in western Turkey. <i>Geology<\/i>, <i>29<\/i>(7), Seiten: 611-614.<\/div>\n  <div class=\"csl-entry\">Gessner, K., Ring, U., Passchier, C. W., G\u00fcng\u00f6r, T. (2001). How to resist subduction : evidence for large-scale out-of-sequence thrusting during Eocene collision in western Turkey. <i>Journal of the Geological Society<\/i>, <i>158<\/i>(5), Seiten: 769-784. <a href=\"http:\/\/dx.doi.org\/10.1144\/jgs.158.5.769\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Bons, P. D., Hilgers, C., Passchier, C. W. (2001). Animations of progressive fibrous vein and fringe formation. <i>Journal of the virtual explorer<\/i>, <i>4<\/i>, Seiten: 25-30.<\/div>\n  <div class=\"csl-entry\">K\u00f6hn, D., Aerden, D. G. A. M., Bons, P. D., Passchier, C. W. (2001). Computer experiments to investigate complex fibre patterns in natural antitaxial strain fringes. <i>Journal of metamorphic geology<\/i>, <i>19<\/i>(2), Seiten: 217-231. <a href=\"http:\/\/dx.doi.org\/10.1046\/j.0263-4929.2000.00305.x\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (2001). Flanking structures. <i>Journal of structural geology<\/i>, <i>23<\/i>(6\/7), Seiten: 951-962. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(00)00166-8\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Piazolo, S., Grotenhuis, S. M. ten, Passchier, C. W. (2001). New apparatus for controlled generalflow modeling of analog materials. In H. Koyi (ed.), <i>Tectonic modeling : a volume in honor of Hans Ramberg<\/i> (pp. Seiten: 235-244). Boulder, Colo.:Geological Society of America. <a href=\"http:\/\/dx.doi.org\/10.1130\/0-8137-1193-2.235\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Zhang, J., Passchier, C. W. (2001). <i>Structural and Metamorphic Evolution of the Archaean High-pressure Granulite in Datong-Huai\u2019an Area, North China An Extentional Collapse and Uplift Model from Structural, Petrological and Palaeomagnetic Investigations<\/i>.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>2000<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Hafner, M., Passchier, C. W. (2000). Development of S-C\u2019 type cleavage in paraffin wax using a circular shear rig. <i>Journal of the virtual explorer<\/i>, <i>2<\/i>, Paper 8. <a href=\"http:\/\/dx.doi.org\/10.3809\/jvirtex.2000.00011\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Hilgers, C., Bons, P. D., Passchier, C. W. (2000). Numerical simulation of fibre growth in antitaxial strain fringes. <i>Journal of structural geology<\/i>, <i>22<\/i>(9), Seiten: 1311-1324. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(00)00039-0\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Koehn, D., Passchier, C. W. (2000). Shear sense indicators in striped bedding-veins. <i>Journal of structural geology<\/i>, <i>22<\/i>(8), Seiten: 1141-1151. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(00)00028-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Trouw, R. A. J., Passchier, C. W., Valeriano, C. M., et al. (2000). Deformational evolution of a cretaceous subduction complex : Elephant Island, South Shetland Islands, Antarctica. <i>Tectonophysics<\/i>, <i>319<\/i>(2), Seiten: 93-110. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(00)00021-4\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1999<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">den Brok, B., Zahid, M., and Passchier, C. W. (1999). Pressure solution compaction of sodium chlorate and implications for pressure solution in NaCl. <i>Tectonophysics<\/i>, <i>307<\/i>(3\/4), Seiten: 297-312. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(99)00103-1\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">den Brok, B., Zahid, M., and Passchier, C. W. (1999). Stress induced grain boundary migration in very soluble brittle salt. <i>Journal of structural geology<\/i>, <i>21<\/i>(2), Seiten: 147-151. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(98)00112-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Ring, U., Gessner, K., Gungor, T., and Passchier, C. W. (1999). The Menderes Massif of western Turkey and the Cycladic Massif in the aegean-do they really correlate?. <i>Journal of the Geological Society<\/i>, <i>156<\/i>(1), Seiten: 3-6. <a href=\"http:\/\/dx.doi.org\/10.1144\/gsjgs.156.1.0003\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1998<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Birtel, S. G., Altenberger, U., and Passchier, C. W. (1998). Multiple deformation and metamorphism of a retrograde ductile shear zone on Holsnoy, Norwegian Caledonides. In U. Kroner (ed.), <i>7. Symposium Tektonik &#8211; Strukturgeologie &#8211; Kristallingeologie : 25. &#8211; 29. M\u00e4rz 1998 in Freiberg<\/i> (pp. Seiten: 36-37). Freiberg:.<\/div>\n  <div class=\"csl-entry\">Birtel, S., Altenberger, U., and Passchier, C. W. (1998). Polyphase structural and metamorphic evolution of the Rossland shear zone at Holsnoy Island, a ductilenappe boundary in the Middle Allochthon of the Norwegian Caledonides. In J. Hofmann (ed.), <i>Symposium Tektonik, Strukturgeologie, Kristallingeologie : TSK VII 1998 in Freiberg\/Sachsen<\/i> (pp. Seiten: 19-44). Stuttgart:Schweizerbart.<\/div>\n  <div class=\"csl-entry\">Den Brok, B., Passchier, C. W., and Sieber, M. (1998). Fibre growth in wet salt aggregates in a temperature gradient field. <i>Mineralogical magazine<\/i>, <i>62<\/i>(4), Seiten: 527-532. <a href=\"http:\/\/rruff.info\/doclib\/MinMag\/Volume_62\/62-4-527.pdf\" title=\"Bibliographical information\" download>Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Den Brok, B., Zahid, M., and Passchier, C. W. (1998). Cataclastic solution creep of very soluble brittle salt as a rock analogue. <i>Earth and planetary science letters<\/i>, <i>163<\/i>(1\/4), Seiten: 83-95. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0012-821X(98)00177-0\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Hetzel, R., Romer, R. L., Candan, O., and Passchier, C. W. (1998). Geology of the Bozdag area, central Menderes massif, sw Turkey : Pan-african basement and alpine deformation. <i>Geologische Rundschau<\/i>, <i>87<\/i>(3), Seiten: 394-406. <a href=\"http:\/\/dx.doi.org\/10.1007\/s005310050218\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1998). Monoclinic model shear zones. <i>Journal of structural geology<\/i>, <i>20<\/i>(8), Seiten: 1121-1137. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(98)00046-7\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1998). Polyphase structural and metamorphic evolution of the Rossland shear zone at Holsnoy Island, a ductile nappe boundary in the Middle Allochton of the Norwegian Caledonides. <i>Zentralblatt f\u00fcr Geologie und Palaeontologie<\/i>, <i>1<\/i>, 19-44.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1998). Structure and crustal thickening of the Menderes Massif, southwest Turkey, and consequences for large-scale correlations between Greece and Turkey. <i>Bulletin of the Geological Society of Greece<\/i>, <i>32<\/i>(1), 145-152.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1998). The late Archaean and early Proterozoic: what happened next?. <i>Netherlands Journal of Geosciences<\/i>, <i>76<\/i>, 357-360.<\/div>\n  <div class=\"csl-entry\">Ten Brink, C. E., and Passchier, C. W. (1998). \uf064-clasts in an experimental mylonite. In <i>Fault-related Rocks A Photographic Atlas<\/i> (pp. 356-358). Princeton University Press.<\/div>\n  <div class=\"csl-entry\">Zegers, T. E., De Keijzer, M., Passchier, C. W., and White, S. H. (1998). The Mulgandinnah Shear Zone : an Archean crustal scale strike-slip zone, eastern Pilbara, western Australia. <i>Precambrian research<\/i>, <i>88<\/i>(1\/4), Seiten: 233-247. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0301-9268(97)00070-3\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1997<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Blom, J. C., Passchier, C. W. (1997). Structures along the Orobic thrust, central Orobic Alps, Italy. <i>Geologische Rundschau<\/i>, <i>86<\/i>(3), Seiten: 627-636. <a href=\"http:\/\/dx.doi.org\/10.1007\/s005310050168\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Dirks, P., Zhang, J. S., Passchier, C. W. (1997). Exhumation of high-pressure granulites and the role of lower crustal advection in the North China Craton near Datong. <i>Journal of structural geology<\/i>, <i>19<\/i>(10), Seiten: 1343-1358. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(97)00044-8\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Druguet, E., Passchier, C. W., Carreras, J., et al. (1997). Analysis of a complex high-strain zone at Cap de Creus, Spain. <i>Tectonophysics<\/i>, <i>280<\/i>(1-2), Seiten: 31-45. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0040-1951(97)00137-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1997). Ductile Extension and Uplift of Granulites in the Datong-Huaian Area, North China. <i>Structural Geology and Geomechanics<\/i>, 173-184.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1997). The fabric attractor. <i>Journal of structural geology<\/i>, <i>19<\/i>(1), Seiten: 113-127. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(96)00077-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Den Brok, S., Van Gool, J., et al. (1997). Laterally constricted shear zone system : the Nordre Stromfjord steep belt, Nagssugtoqidian Orogen, W Greenland. <i>Terra nova<\/i>, <i>9<\/i>(5\/6), Seiten: 199-202. <a href=\"http:\/\/dx.doi.org\/10.1111\/j.1365-3121.1997.tb00012.x\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Trouw, R., Passchier, C. W., Simoes, L., et al. (1997). Mesozoic tectonic evolution of the South Orkney microcontinent, Scotia arc, Antarctica. <i>Geological magazine<\/i>, <i>134<\/i>(3), Seiten: 383-401. <a href=\"http:\/\/dx.doi.org\/10.1017\/S0016756897007036\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1996<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1996). Metasomatic tourmalinite formation along basement-cover d\u00e9collements, Orobic Alps, Italy. <i>Schweizerische Mineralogische und Petrographische Mitteilungen<\/i>, <i>76<\/i>, 193-207.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Trouw, R. A. J. (1996). <i>Microtectonics<\/i> (p. 289 S.). Berlin:Springer.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Williams, P. R. (1996). Conflicting shear sense indicators in shear zones : the problem of non-ideal sections. <i>Journal of structural geology<\/i>, <i>18<\/i>(10), Seiten: 1281-1284. <a href=\"http:\/\/dx.doi.org\/10.1016\/S0191-8141(96)00051-X\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Slack, J. F., Passchier, C. W., Zhang, J. S. (1996). Metasomatic tourmalinite formation along basement-cover decollements, Orobic Alps, Italy. <i>Schweizerische mineralogische und petrographische mitteilungen<\/i>, <i>76<\/i>(2), Seiten: 193-207. <a href=\"http:\/\/retro.seals.ch\/digbib\/view2?pid=smp-001:1996:26::208\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Westaway, R., Hetzel, R., Passchier, C. W., et al. (1996). Bivergent extension in orogenic belts: The Menderes massif (southwestern Turkey): Comment and Reply. <i>Geology<\/i>, <i>24<\/i>(1), 93-93. <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1996)024<0093:beiobt>2.3.co;2&#8243; title=&#8221;Bibliographical information&#8221;>DOI<\/a> <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1996)024%3C0093:beiobt%3E2.3.co;2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Zuijderwijk, M. J., White, S. H., Passchier, C. W. (1996). Shear zone reactivation studies in the Vestfold Hills, East Antarctica. <i>Circumpolar journal<\/i>, <i>11<\/i>(1\/2), Seiten: 69-71.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>1995<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Hanmer, S., and Passchier, C. (1995). Kinematic analysis \u2014 the sense of shear\u2010sense. Discussion of: \u2018Essay Review: Kinematic analysis \u2014 pure nonsense or simple nonsense\u2019 by D. Flinn. <i>Geological Journal<\/i>, <i>30<\/i>(2), 197-198. <a href=\"https:\/\/doi.org\/10.1002\/gj.3350300210\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Hetzel, R., Passchier, C. W., Ring, U., and Dora, O. O. (1995). Bivergent extension in orogenic belts : the Menderes Massif (southwestern turkey). <i>Geology<\/i>, <i>23<\/i>(5), Seiten: 455-458.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1995). Precambrian orogenesis &#8211; was it really different. <i>Netherlands Journal of Geosciences<\/i>, <i>74<\/i>, 141-150.<\/div>\n  <div class=\"csl-entry\">Tenbrink, C. E., and Passchier, C. W. (1995). Modeling of mantled porphyroclasts using non-newtonian rock analog materials. <i>Journal of structural geology<\/i>, <i>17<\/i>(1), Seiten: 131-146. <a href=\"http:\/\/dx.doi.org\/10.1016\/0191-8141(94)E0032-T\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1994<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W., and Speck, P. J. H. R. (1994). The kinematic interpretation of obliquely-transected porphyroblasts: an example from the Trois Seigneurs Massif, France. <i>International Journal of Rock Mechanics and Mining Sciences &amp;amp; Geomechanics Abstracts<\/i>, <i>31<\/i>(6), 265-265. <a href=\"https:\/\/doi.org\/10.1016\/0148-9062(94)90035-3\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., and Speck, P. J. H. R. (1994). The kinematic interpretation of obliquely-transected porphyroblasts: an example from the Trois Seigneurs Massif, France. <i>Journal of Structural Geology<\/i>, <i>16<\/i>(7), 971-984. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(94)90079-5\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1994). Structural geology across a proposed Archaean terrane boundary in the eastern Yilgarn craton, Western Australia. <i>Precambrian Research<\/i>, <i>68<\/i>(1-2), 43-64. <a href=\"https:\/\/doi.org\/10.1016\/0301-9268(94)90064-7\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Zhang, J. S., Passchier, C. W., Slack, J. F., et al. (1994). Cryptocrystalline Permian tourmalinites of possible metasomatic origin in the Orobic Alps, northern Italy. <i>Economic Geology<\/i>, <i>89<\/i>(2), 391-396. <a href=\"https:\/\/doi.org\/10.2113\/gsecongeo.89.2.391\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Jiasheng, Z., Dirks, P. H. G. M., Passchier, C. W. (1994). Extensional collapse and uplift in a polymetamorphic granulite terrain in the Archaean and Palaeoproterozoic of north China. <i>Precambrian Research<\/i>, <i>67<\/i>(1-2), 37-57. <a href=\"https:\/\/doi.org\/10.1016\/0301-9268(94)90004-3\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1994). Mixing in flow perturbations : a model for development of mantled porphyroclasts in mylonites. <i>Journal of structural geology<\/i>, <i>16<\/i>(5), Seiten: 733-736. <a href=\"http:\/\/dx.doi.org\/10.1016\/0191-8141(94)90123-6\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1993<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Sliding-scale Mohr diagram. (1993). <i>International Journal of Rock Mechanics and Mining Sciences &amp;amp; Geomechanics Abstracts<\/i>, <i>30<\/i>(5), 301-301. <a href=\"https:\/\/doi.org\/10.1016\/0148-9062(93)92485-9\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Bons, P. D., Jesseli, M. W., and Passchier, C. W. (1993). The analysis of progressive deformation in rock analogues. <i>Journal of Structural Geology<\/i>, <i>15<\/i>(3-5), 403-411. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(93)90136-x\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1993). The sliding-scale Mohr diagram. <i>Tectonophysics<\/i>, <i>218<\/i>(4), 367-373. <a href=\"https:\/\/doi.org\/10.1016\/0040-1951(93)90325-e\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., and Sokoutis, D. (1993). Experimental modeling of mantled porphyroclasts. <i>Journal of structural geology<\/i>, <i>15<\/i>(7), Seiten: 895-909. <a href=\"http:\/\/dx.doi.org\/10.1016\/0191-8141(93)90183-B\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., and ten Brink, C. D. (1993). \u03b4 objects as a gauge for stress sensitivity of strain rate in mylonites. <i>Earth and planetary science letters<\/i>, <i>120<\/i>(3\/4), Seiten: 239-245. <a href=\"http:\/\/dx.doi.org\/10.1016\/0012-821X(93)90242-2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1992<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">PASSCHIER, C. W., TROUW, R. A. J., ZWART, H. J., and VISSERS, R. L. M. (1992). Porphyroblast rotation: &lt;i&gt;eppur si muove&lt;\/i&gt;&lt;i&gt;*&lt;\/i&gt;&lt;i&gt;?&lt;\/i&gt;. <i>Journal of Metamorphic Geology<\/i>, <i>10<\/i>(3), 283-294. <a href=\"https:\/\/doi.org\/10.1111\/j.1525-1314.1992.tb00083.x\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1991<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W., Bekendam, R. F., Hoek, J. D., et al. (1991). Proterozoic geological evolution of the northern Vestfold Hills, Antarctica. <i>Geological Magazine<\/i>, <i>128<\/i>(4), 307-318. <a href=\"https:\/\/doi.org\/10.1017\/s0016756800017581\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1991). The classification of dilatant flow types. <i>Journal of Structural Geology<\/i>, <i>13<\/i>(1), 101-104. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(91)90105-r\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Hanmer, S., Passchier, C. W. (1991). <i>Shear-sense Indicators A Review<\/i>. Geological Survey of Canada.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1991). Deformation in the Revenue granite pluton, Mt Isa Inlier, Australia. <i>Netherlands Journal of Geosciences<\/i>, <i>70<\/i>, 275-285.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1991). Geometric constraints on the development of shear bands in rocks. <i>Netherlands Journal of Geosciences<\/i>, <i>70<\/i>, 203-211.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>1990<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1990). Reconstruction of deformation and flow parameters from deformed vein sets. <i>Tectonophysics<\/i>, <i>180<\/i>(2-4), 185-199. <a href=\"https:\/\/doi.org\/10.1016\/0040-1951(90)90307-t\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., Hoek, J. D., Bekendam, R. F., and De Boorder, H. (1990). Ductile reactivation of Proterozoic brittle fault rocks; an example from the Vestfold Hills, East Antarctica. <i>Precambrian Research<\/i>, <i>47<\/i>(1-2), 3-16. <a href=\"https:\/\/doi.org\/10.1016\/0301-9268(90)90026-m\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1990). A Mohr circle construction to plot the stretch history of material lines. <i>Journal of Structural Geology<\/i>, <i>12<\/i>(4), 513-515. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(90)90038-z\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1989<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W., and Williams, P. R. (1989). Proterozoic extensional deformation in the Mount Isa inlier, Queensland, Australia. <i>Geological Magazine<\/i>, <i>126<\/i>(1), 43-53. <a href=\"https:\/\/doi.org\/10.1017\/s0016756800006130\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1989). Alternating brittle and ductile deformation in the Archaean basement of the Vestfold Hills, Antarctica. <i>circumpolar Journal<\/i>, <i>4<\/i>, 18-24.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>1988<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1988). The use of Mohr circles to describe non-coaxial progressive deformation. <i>Tectonophysics<\/i>, <i>149<\/i>(3-4), 323-338. <a href=\"https:\/\/doi.org\/10.1016\/0040-1951(88)90181-3\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1988). Analysis of deformation paths in shear zones. <i>Geologische Rundschau<\/i>, <i>77<\/i>(1), 309-318. <a href=\"https:\/\/doi.org\/10.1007\/bf01848692\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., and Urai, J. L. (1988). Vorticity and strain analysis using Mohr diagrams. <i>Journal of Structural Geology<\/i>, <i>10<\/i>(7), 755-763. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(88)90082-x\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1987<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1987). Efficient use of the velocity gradients tensor in flow modelling. <i>Tectonophysics<\/i>, <i>136<\/i>(1-2), 159-163. <a href=\"https:\/\/doi.org\/10.1016\/0040-1951(87)90338-6\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1987). Comment and Reply on \u201cEvidence for early extensional tectonics in the Proterozoic Mount Isa inlier, Australia\u201d. <i>Geology<\/i>, <i>15<\/i>(10), 977-977. <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1987)15<977:caroef>2.0.co;2&#8243; title=&#8221;Bibliographical information&#8221;>DOI<\/a> <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1987)15%3C977:caroef%3E2.0.co;2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1987). Stable positions of rigid objects in non-coaxial flow\u2014a study in vorticity analysis. <i>Journal of Structural Geology<\/i>, <i>9<\/i>(5-6), 679-690. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(87)90152-0\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1986<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1986). Flow in natural shear zones\u2014the consequences of spinning flow regimes. <i>Earth and Planetary Science Letters<\/i>, <i>77<\/i>(1), 70-80. <a href=\"https:\/\/doi.org\/10.1016\/0012-821x(86)90133-0\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W., and Simpson, C. (1986). Porphyroclast systems as kinematic indicators. <i>Journal of Structural Geology<\/i>, <i>8<\/i>(8), 831-843. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(86)90029-5\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1986). Evidence for early extensional tectonics in the Proterozoic Mount Isa inlier, Australia. <i>Geology<\/i>, <i>14<\/i>(12), 1008-1008. <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1986)14<1008:efeeti>2.0.co;2&#8243; title=&#8221;Bibliographical information&#8221;>DOI<\/a> <a href=\"https:\/\/doi.org\/10.1130\/0091-7613(1986)14%3C1008:efeeti%3E2.0.co;2\" title=\"Bibliographical information\" >Author\/Publisher URL<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1985<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1985). Water-deficient mylonite zones \u2014 An example from the Pyrenees. <i>Lithos<\/i>, <i>18<\/i>, 115-127. <a href=\"https:\/\/doi.org\/10.1016\/0024-4937(85)90014-3\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1984<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1984). Mylonite-dominated footwall geometry in a shear zone, central Pyrenees. <i>Geological Magazine<\/i>, <i>121<\/i>(5), 429-436. <a href=\"https:\/\/doi.org\/10.1017\/s0016756800029964\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1984). The generation of ductile and brittle shear bands in a low-angle mylonite zone. <i>Journal of Structural Geology<\/i>, <i>6<\/i>(3), 273-281. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(84)90051-8\" title=\"Bibliographical information\">DOI<\/a><\/div>\n  <div class=\"csl-entry\">Passchier, C. W. (1984). Fluid inclusions associated with the generation of pseudotachylyte and ultramylonite in the French Pyr\u00e9n\u00e9es. <i>Bulletin de Min\u00e9ralogie<\/i>, <i>107<\/i>(2), 307-315. <a href=\"https:\/\/doi.org\/10.3406\/bulmi.1984.7760\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1983<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1983). The reliability of asymmetric c-axis fabrics of quartz to determine sense of vorticity. <i>Tectonophysics<\/i>, <i>99<\/i>(1), T9-T18. <a href=\"https:\/\/doi.org\/10.1016\/0040-1951(83)90166-x\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1982<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C. W. (1982). Pseudotachylyte and the development of ultramylonite bands in the Saint-Barth\u00e9lemy Massif, French Pyrenees. <i>Journal of Structural Geology<\/i>, <i>4<\/i>(1), 69-79. <a href=\"https:\/\/doi.org\/10.1016\/0191-8141(82)90008-6\" title=\"Bibliographical information\">DOI<\/a><\/div>\n<\/div>\t\n<\/div>\n\n<h3>1981<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\">Passchier, C., and Passchier, C. W. (1981). Structural geology of the central Sesia-Lanzo Zone. <i>Netherlands Journal of Geosciences<\/i>, <i>60<\/i>, 497-507.<\/div>\n<\/div>\t\n<\/div>\n\n<h3>Not dated<\/h3>\n\t<div>\n\n\t\n\t<div class=\"csl-bib-body\">\n  <div class=\"csl-entry\"><i>Geologia de Campo de Terrenos Gn\u00e1issicos de Alto Grau<\/i>. EdUSP.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. Mylonites in the continental crust and their role as seismic reflectors. <i>Netherlands Journal of Geosciences<\/i>, <i>65<\/i>, 167-176.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. Mylonitic deformation in the Saint Barth\u00e9lemy Massif, French Pyrenees, with emphasis on the genetic relationship between ultramylonite and pseudotachylyte. <i>GUA Papers of Geology<\/i>, <i>16<\/i>, 1-173.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. Proterozoic deformation in the Duchess Belt, Australia: a contribution to the BMR Mount Isa Regional Tectonic History Program. <i>Netherlands Journal of Geosciences<\/i>, <i>65<\/i>, 47-56.<\/div>\n  <div class=\"csl-entry\">Passchier, C. W. 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The Geoarchaeology Work Group in Mainz focuses primarily on the ancient culture of the Mediterranean region, particularly the Roman period. We specialize in researching ancient water supply systems such as aqueducts and the application of geological methods in antiquity. Our main task is the investigation &hellip; <a href=\"https:\/\/www.geowiss.uni-mainz.de\/en\/institut-fuer-geowissenschaften\/geoarchaeologie\/\">Continued<\/a><\/p>\n","protected":false},"author":2181,"featured_media":0,"parent":21238,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"categories":[143],"tags":[146],"class_list":["post-21704","page","type-page","status-publish","hentry","category-work-groups","tag-geoarchaeology-work-group"],"content_raw":"<!-- wp:jgu\/anchornavigation \/--><!-- wp:jgu\/teaserbox {\"headline\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"image\":{\"id\":9757,\"url\":null},\"color\":\"red\",\"index\":\"Research group\",\"title\":\"\\u003cstrong\\u003eGeoarchaeology\\u003c\/strong\\u003e\",\"excerpt\":\"\\u003cstrong\\u003eWe reconstruct the function of ancient water supply systems such as aqueducts based on the composition of carbonate deposits, using geological methods in antiquity.\\u003c\/strong\\u003e\"} \/--><!-- wp:jgu\/heading {\"index\":\"AG\",\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Geoarchaeology\"} \/--><!-- 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\">Geoarchaeology is the application of geological knowledge to archaeological sites. The Geoarchaeology Work Group in Mainz focuses primarily on the ancient culture of the Mediterranean region, particularly the Roman period. We specialize in researching ancient water supply systems such as aqueducts and the application of geological methods in antiquity. Our main task is the investigation of calcareous deposits in ancient aqueducts, water mills, lifting installations, and baths using fabric analysis and geochemical procedures. From these deposits, we obtain information about ancient water management, societal changes, the environment and climate of antiquity, as well as earthquakes. In addition to this core area, we research the use of building stones and quarrying operations in antiquity, the properties of Roman concrete, and attempt to reconstruct the understanding of geology and engineering among prospectors, architects, and engineers of antiquity.     <\/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\":13031},\"caption\":\"Aqua Marcia, Rome\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><!-- 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\":9769},{\"url\":null,\"id\":9757},{\"url\":null,\"id\":13031},{\"url\":null,\"id\":14302},{\"url\":null,\"id\":14300},{\"url\":null,\"id\":11575},{\"url\":null,\"id\":14303}],\"thumbsPosition\":\"bottom\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><\/div>\n<!-- \/wp:group --><!-- wp:jgu\/section {\"color\":\"white-dark-text\",\"metadata\":{\"name\":\"Forschung\"}} -->\n<div class=\"jgu-bgsection bg bg-white-dark-text \"><div class=\"content padding-medium\"><!-- wp:jgu\/anchorpoint {\"title\":\"Research\",\"slug\":\"research\"} \/-->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Research\"} \/-->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14300},\"caption\":\"Replica of a Roman saw\"} \/-->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 1\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/hygienische-bedingungen-in-pompejis-fruehen-baedern-waren-schlecht\/\"><strong>Hygienic conditions in Pompeii's early baths were poor<\/strong><\/a> Calcareous deposits in wells, pipes, and bathing facilities provide insights into Pompeii's ancient water supply<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":11575}} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 2\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/das-wassermanagement-des-antiken-arles\/\"><strong>The water management of ancient Arles<\/strong><\/a> Using carbonate fragments, researchers from Mainz, Oxford, and Innsbruck have deciphered the complex history of the aqueduct system of Arles<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14345},\"caption\":\"Aqueduct of Arles\"} \/-->\n\n<!-- wp:paragraph {\"fontSize\":\"normal\"} -->\n<p class=\"has-normal-font-size\"><\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 3\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/unbekannte-mikroorganismen-nutzten-marmor-und-kalkstein-als-lebensraum\/\"><strong>Unknown microorganisms used marble and limestone as habitat<\/strong><\/a> Unusual structures are noticeable in the rock of desert regions, whose origin has not been clarified<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14347},\"caption\":\"Marble sample from Namibia\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 4\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/karbonatschichten-eroeffnen-blick-in-die-roemerzeit\/\"><strong>Carbonate layers open a view into the Roman era<\/strong><\/a> Researchers reconstruct the developmental history of the water mills of Barbegal through carbonate deposits<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14350},\"caption\":\"Cross-section of a carbonate fragment from the mills of Barbegal\"} \/-->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 5\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/regelmaessige-reinigung-hat-wasserversorgung-ueber-roemischen-aquaedukt-von-divona-gesichert\/\"><strong>Regular cleaning secured water supply via the Roman aqueduct of Divona<\/strong><\/a> Calcareous deposits in the water channel were systematically removed \/ Maintenance in accordance with Roman recommendations<\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14351},\"caption\":\"Masonry channel with Opus Signinum as water protection\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 6\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/der-aquaedukt-von-konstantinopel-wie-der-laengste-wasserkanal-der-antike-gewartet-wurde\/\"><strong>The aqueduct of Constantinople: How the longest water channel of antiquity was maintained<\/strong><\/a> Double water channels possibly served to maintain the facility during ongoing operation <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14357},\"caption\":\"Two-story Kur\u015funlugerme Bridge of the aqueduct of Constantinople\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n\n<!-- wp:columns {\"metadata\":{\"name\":\"Projekt 7\"},\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"44.45%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:44.45%\"><!-- wp:list -->\n<ul class=\"wp-block-list\"><!-- wp:list-item {\"translatedWithWPMLTM\":\"1\"} -->\n<li><a href=\"https:\/\/presse.uni-mainz.de\/materialverlust-bei-der-produktion-von-marmorplatten-war-in-der-roemischen-kaiserzeit-womoeglich-niedriger-als-heute\/\"><strong>Material loss in the production of marble slabs was possibly lower in the Roman Imperial period than today<\/strong><\/a> Analysis of wall cladding from the 2nd century provides new insights into marble extraction and processing <\/li>\n<!-- \/wp:list-item --><\/ul>\n<!-- \/wp:list --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"22.22%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:22.22%\"><!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14360},\"caption\":\"A pair of marble slabs in typical, mirror-reversed arrangement\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><\/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\":\"674\",\"organizationId\":974,\"roleId\":13} \/-->\n\n<!-- wp:jgu\/button -->\n<!-- wp:jgu\/button-item {\"text\":\"Research profile\",\"link\":{\"url\":\"https:\/\/www.geosciences.uni-mainz.de\/univ-prof-dr-cees-passchier\/\",\"linkTarget\":\"\",\"rel\":\"\",\"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\/contact-card {\"name\":\"S\u00fcrmelihindi, G\u00fcl\",\"avatar\":{\"id\":null,\"url\":null,\"credit\":\"\"}} -->\n<!-- wp:jgu\/list-item {\"icon\":\"address-card-solid\",\"title\":\"Research Assistant\",\"uuid\":\"1773144921640\"} \/-->\n\n<!-- wp:jgu\/list-item {\"icon\":\"university-solid\",\"title\":\"Geoarchaeology\",\"uuid\":\"1773144984525\"} -->\n<!-- wp:jgu\/list-item {\"uuid\":\"1773738866122\"} \/-->\n<!-- \/wp:jgu\/list-item -->\n<!-- \/wp:jgu\/contact-card -->\n\n<!-- wp:spacer {\"height\":\"10px\"} -->\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer --><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person \/--><\/div>\n<!-- \/wp:column -->\n\n<!-- wp:column {\"width\":\"100%\"} -->\n<div class=\"wp-block-column\" style=\"flex-basis:100%\"><!-- wp:jgu\/idm-person \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns --><\/div><\/div>\n<!-- \/wp:jgu\/section --><!-- wp:jgu\/section {\"color\":\"white-dark-text\",\"metadata\":{\"name\":\"Labore\"}} -->\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\"><\/div>\n<!-- \/wp:group -->\n\n<!-- wp:jgu\/heading {\"tags\":{\"htmlTag\":\"h2\",\"classTag\":\"\",\"tag\":\"h2\"},\"heading\":\"Laboratories\\u003cbr\\u003e\",\"className\":\"alignwide\"} \/-->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">We use other laboratories for our research work<\/p>\n<!-- \/wp:paragraph --><\/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 {\"image\":{\"url\":null,\"id\":14309},\"caption\":\"Microtectonics Masterclass at JGU Mainz\"} \/-->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><strong>Next class in Mainz will be from 17.2.2026 to 26.2.2026<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><em>It is possible to participate in only Part I (17th-21st of February) or Part II (23rd-26th of February) of the Microtectonics Masterclass, but we recommend joining both since they are complimentary. We invite participants external to the University of Mainz to join us for the classes, for a fee detailed below.  <\/em><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>If you want to register, or have any questions, please send an <a href=\"mailto:hawemann@uni-mainz.de\">e-mail<\/a> to Friedrich Hawemann.<\/strong><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\">We offer two linked <strong>practical Masterclasses in Microtectonics<\/strong> at the University of Mainz, Germany. These courses should interest students, postdocs and professionals who wish to learn about the deformation of rocks on the microscopic scale. <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/tabs {\"metadata\":{\"name\":\"Lehrveranstaltungen\"}} -->\n<!-- wp:jgu\/tabs-item {\"title\":\"Masterclass Microtectonics\",\"slug\":\"masterclass-microtectonics\",\"metadata\":{\"name\":\"MSc class\"}} -->\n<!-- wp:columns {\"className\":\"\"} -->\n<div class=\"wp-block-columns\"><!-- wp:column -->\n<div class=\"wp-block-column\"><!-- wp:paragraph -->\n<p class=\"has-big-font-size\">Masterclass Microtectonics<\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>Part I:<\/strong> Delivered by <strong>Prof. Virginia Toy<\/strong> and <strong>Dr. Friedrich Hawemann<\/strong>, which is entitled \"Fault Rocks and Fault Mechanisms Revisited\" will focus on how fault zone processes can be inferred from their textural record. The class will examine the set of thin sections and samples of fault rocks (mylonites, cataclasites, pseudotachylytes) from the Outer Hebrides Fault Zone (Scotland) that inspired Sibson (1977) to develop his widely-cited classification of fault rocks, and from New Zealand's Alpine Fault Zone where he next applied this classification. Additionally, a set of exercises will examine microstructural datasets from both Outer Hebrides and Alpine Fault Zone samples acquired using advanced analytical tools, including SEM (EBSD, BSE-imaging), TEM, and synchrotron-CT. These exercises will demonstrate how to quantify the 2D and 3D arrangement and shapes of fault rock grains and particles, their textures, their crystallographic orientations, and the nature of porosity. The implications for fault rheology will be explored.    <\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph {\"translatedWithWPMLTM\":\"1\"} -->\n<p class=\"has-big-font-size\"><strong>Part II:<\/strong> Delivered by <strong>Prof. Cees Passchier<\/strong>, teaches how deformation mechanisms can be inferred from the microstructures visible in thin sections. It is based on the book \"Microtectonics\" by Passchier and Trouw (2005), and the superb Microtectonics Collection of 300 selected thin sections that are the source of figures in that book will be examined during the course. The main topics, which are treated through an alternation of lectures and microscopy practicals, are: Principles of microtectonic analysis, overprinting relations, deformation phases and tectonic phases, flow and deformation, intracrystalline deformation, foliations and lineations, shear zones, veins and fringes, porphyroblasts, metamorphic reaction rims.  <\/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\":14375},\"caption\":\"Deformation structure\"} \/-->\n\n<!-- wp:spacer {\"height\":\"164px\"} -->\n<div style=\"height:164px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<!-- \/wp:spacer -->\n\n<!-- wp:jgu\/image {\"image\":{\"url\":null,\"id\":14372},\"caption\":\"Crystallite in fissure mineralization\"} \/--><\/div>\n<!-- \/wp:column --><\/div>\n<!-- \/wp:columns -->\n<!-- \/wp:jgu\/tabs-item -->\n<!-- \/wp:jgu\/tabs -->\n\n<!-- wp:separator -->\n<hr class=\"wp-block-separator has-alpha-channel-opacity\" \/>\n<!-- \/wp:separator -->\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\":14408}} \/-->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:paragraph -->\n<p class=\"has-big-font-size\"><\/p>\n<!-- \/wp:paragraph -->\n\n<!-- wp:jgu\/fis {\"groupBy\":\"year\",\"user\":\"cpasschi\"} \/--><\/div><\/div>\n<!-- 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