Kontakt Information

We are always happy to have visitors. Follow the directions to the university of Mainz, after which you can find us in the building "Naturwiss.- Institutsgeb." on this map. We are located on the ground and first floor in the offices listed below. 


Arbeitsgruppenleiter

06131/39-

Raum

E-Mail

Univ.-Prof. Dr.
Kaus, Boris
24527 00-285 kaus@uni-mainz.de
Wissenschaftliches Personal

06131/39-

Raum

E-Mail

Dr.
Boutonnet, Emmanuelle
22850 00-264 boutonne@uni-mainz.de
Dr.
Deckert, Hagen
26594 02-542 deckert@uni-mainz.de
Dr.
Popov, Anton
23247 00-265 popov@uni-mainz.de
Dr.
Richard, Guillaume
00-275 richarg@uni-mainz.de
Doktoranden

06131/39-

Raum

E-Mail

Dipl.-Geophys.
Baumann, Tobias
20941 00-261 baumann@uni-mainz.de
Dipl.-Geol.
Fernandez, Naiara
20941 00-261 fernande@uni-mainz.de
Dipl.-Geol.
Malm, Florian
25225 02-540 malmf@uni-mainz.de
Dipl.-Geol.
Püsök, Adina
22850 00-264 puesoek@uni-mainz.de
Dipl.-Math.
Lehmann, Ragnar
23247 00-265 r.lehmann@uni-mainz.de
Externe Doktoranden

06131/39-

Raum

E-Mail

BSc. Geol.
Cao, Wenrong
wenrongc@usc.edu
Dipl.-Geol.
Collignon, Marine
marine.collignon@erdw.ethz.ch
MSc.
Ruh, Jonas
jonas.ruh@erdw.ethz.ch
Dipl. Geoph.
Thielmann, Marcel
thielmann@erdw.ethz.ch
Ehemalige Mitarbeiter

06131/39-

Raum

E-Mail

Dr.
Bock, Melanie
22850 00-264 bockme@uni-mainz.de
Univ.-Prof. Dr. (im Ruhestand)
Jacoby, Wolfgang
jacoby@uni-mainz.de
MSc. Geophysics
Keller, Tobias
keller@erdw.ethz.ch
MSc.
Lechmann, Sarah
sarah.lechmann@erdw.ethz.ch
Dr.
Sebazungu, Evariste
sebazung@uni-mainz.de

Diplomanden

 Ulrich Kelka

 Erik Schaefer

 Oliver Hartkorn

 B.Sc. Studenten

 Fee Arens

News:


Our latest 4 publications:

  • Given the correct parameters, shear heating results in lithospheric-scale shear zones. But does this result in a subduction zone? Read more...
  • Fold and thrust-belts have a large variety of deformation styles. We show that this might be caused by thin weak layers. Read more...
  • On Earth, all lithospheric plates move westwards (relative to the lower mantle). But why?
  • Under which conditions can we use 'sticky-air' to model a free surface?

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