Institut für Geologie

© B. Grasemann

Research at the Department of Geology focuses on pure and applied research into both ductile/brittle lithospheric and Earth-surface processes. Field-based geology and quantitative modeling of geodynamic processes form the foundation of academic and applied Earth sciences research, in particular in petroleum geology and seismology. A close collaboration between research groups focuses on integrated geodynamics/tectonics and sedimentology/stratigraphy.

Institutsleitung: Daniel Le Heron, Bernhard Grasemann (Stv.), Michael Wagreich (Stv)

 Neuigkeiten und Veranstaltungen

Oktober 2024

Erdwissenschaftliches Kolloquium

Nächster Vortrag: 17. Oktober, 17:00 c.t., HS 2
Peter Krois (deeep Tiefengeothermie GmbH)

Oktober 2024

Wolfgang Schollnberger Masters Thesis Prizes

We recently held a prize giving for our three recipients of the Masters Thesis Prize: Sabine Wimmer, Jaqueline Krivetz and Lino Eggerth. Congratulations!

August 2024

Neue Publikation/Presse

Was ein Salzriese mit dem beinahe-Reset allen Lebens im Mittelmeer zu tun hat
Konstantina Agiadi

Juli 2024

Zertifikat

Paper published by Michael Wagreich as co-author in Journal of Quaternary Science on behalf of Quaternary Research Association, is one of the top 10 most-cited papers published 1st January 2022 – 31st December 2023. https://doi.org/10.1002/jqs.3467

Juni 2024

Podcast

Was die Donau über die Menschheit zu erzählen weiß
Diana Hatzenbühler

Mai 2024

Presse/Gastkommentar

Der falsche Abgesang auf das Anthropozän
Robert Braun, Michael Wagreich

Februar 2024

Ö1 Radiokolleg Anthropozän

Anthropozän - Das Zeitalter des Menschen (2)
Diana Hatzenbühler, Michael Weißl

Februar 2024

Artikel/Presse

„Menschenzeitalter“ bleibt umstritten
Michael Wagreich, Christian Köberl

Jänner 2024

Neue Publikation/Presse

Neue Publikation in „Sedimentology“:
Stephanie Neuhuber, Susanne Gier, Erich Draganits, Peter Steier, Monika Bolka, Franz Ottner, Christoph Spötl, Dorothee Hippler, Patrick Meister: Radiocarbon ages of microcrystalline authigenic carbonate in Lake Neusiedl (Austria) suggest millennial-scale growth of Mg-calcite and protodolomite. (doi: 10.1111/sed.13161)