The central research theme of our section is the understanding of the physical and physico-chemical processes that determine the dynamics and mechanical properties of the Earth's crust and upper mantle. The topics range from geomechanics and rock physics to the deformation behavior of the lithosphere, covering scales from the laboratory (micrometer to centimeter) to mines and boreholes (decimeter to dekameter), geo-reservoirs, and those of tectonic processes (kilometer scale and beyond). Our goal is to develop a quantitative, scale-bridging understanding of the mechanics of deformation and material transport processes in the lithosphere, their changes in time and space, and from brittle to ductile behavior.
Scientific drilling is an important method in this context, as it provides undisturbed material in the form of core samples and formation fluids, enabling geophysical measurements and various long-term studies under in-situ conditions across scales. In our laboratories, we conduct experiments on deformation and transport processes in reservoir and surrounding rock. We study seismic and aseismic deformation processes under high pressures and temperatures, deriving principles that we apply under natural conditions in geological reservoirs or along tectonic plate boundaries. Additionally, we measure processes before, during, and after earthquakes of varying magnitudes in tectonically active regions, both on the Earth's surface and underground. Our research provides the physical foundations for assessing geohazards and addressing geomechanical questions related to the exploration and utilization of the subsurface.
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Seismomechanics and Slip Transients Team lead:-
Prof. Dr. Patricia Martinez Garzon4.2 Geomechanics and Scientific Drilling
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Scientific Drilling Team lead:-
Dr. Thomas Wiersberg4.2 Geomechanics and Scientific Drilling
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Underground Seismics Team lead: -
Physics of Rock Deformation and Faulting Team lead: -
Experimental Rheology & Metamorphism Team lead: -
High Pressure Workshop Team lead:
All GFZ job offers
Possible doctoral and master's theses as well as all student internships offered at the GFZ can also be found under the link above.
![[Translate to English:] Fieldwork](/fileadmin/_processed_/c/4/csm_IMG-20230331-WA0008_f2bb58bfb7.jpeg)
![[Translate to English:] [Translate to English:] ICDP Bohrung an der Alpine Fault in Neuseeland](/fileadmin/_processed_/2/5/csm_5_New_Zealand_Alpine_Fault_Drilling_2_Credits_TWiersberg_klein_fcf53531d2.jpeg)
![[Translate to English:] Active seismic measurement in a salt mine (Germany) with the components seismic source, control unit and data storage for exploring the salt rock in the vicinity of a cavernous structure.](/fileadmin/_processed_/e/2/csm_P1000900a_3ff1ffcb68.jpeg)
![[Translate to English:] [Translate to English:] Mikrostruktur einer im Labor erzeugten Verwerfungszone in Granit. Brantut, N., Dilatancy-induced fluid pressure drop during dynamic rupture: Direct experimental evidence and consequences for earthquake dynamics, Earth Planet. Sci. Lett., 538, 116179, <doi:10.1016/j.epsl.2020.116179>](/fileadmin/_processed_/d/d/csm_Nicolas_granite_c728290206.png)
![[Translate to English:] [Translate to English:] Unter Eklogit-Fazies-Bedingungen, d. h. unter Druck- und Temperaturbedingungen, die in der verdickten unteren kontinentalen Kruste vorherrschen, zerfällt Plagioklas bei Vorhandensein selbst geringer Mengen an Flüssigkeiten leicht und bildet stabile Phasen wie Zoisit. Letzteres ist ein wasserhaltiges Mineral und bildet winzige Nadeln innerhalb und entlang von Plagioklas-Körnern. Die Fülle dieser Zoisitnadeln, hauptsächlich in Körnern auf der linken Seite des Bildes, erweckt den Eindruck von Schattierungen, die die Körner bedecken. Wir wollen besser verstehen, wie sich der Abbau von Plagioklas auf die Festigkeit der unteren kontinentalen Kruste auswirken kann, indem wir die Details und Raten dieser Hydratationsreaktion untersuchen. Das Bild wurde in gekreuztem polarisiertem Licht mit einer Lambda-Platte einer Anorthosit-Handprobe aufgenommen, die auf Holsnøy (SW-Norwegen) gesammelt wurde.](/fileadmin/_processed_/4/2/csm_HydrationPlg_new_87f917474b.png)