Our aim is to improve the understanding of geodynamic processes operating inside the solid Earth and their surface manifestation at a broad range of spatial and temporal scales through advanced numerical modeling. Our research focii are located at both plate boundaries and within the plate interiors, inside the deep mantle and at the surface. We constrain our models by multidisciplinary surface observations acquired by the GFZ and the international scientific community and look for practical applications of fundamental research, like tsunami early warning and hazard assessment. To approach our aims, we develop our own numerical methods and tools, but also extensively employ and co-develop numerical techniques provided by the international community.
European Research Council Synergy Grant 2019 MEET Funded
An ERC (European Research Council) Synergy grant of €12.8 million over six years (2020-2026) has been awarded to Alexander Sobolev (IsTerre, Grenoble), Stephan Sobolev (GFZ Potsdam, Germany) and John Valley (University of Wisconsin, Madison, USA) to study the evolution of Earth’s chemical composition and the underlying physical processes from 4.4 billion years ago to present in a project entitled “Monitoring Earth Evolution through Time” (MEET).
June 2019 - Our article in Nature suggests that emergence and evolution of plate tectonics on Earth was controlled not only by deep processes like mantle convection and secular cooling of the mantle but also by major surface erosion events. The eroded massive continental sediments acted as a lubricant for subducting slabs thus stabilizing subduction and activating plate tectonics a number of times in Earth’s history since about 3 Ga. The largest surface erosion event possibly related to ‘Snowball Earth’ glaciations at 0.7-0.6 Ga produced the global geological boundary called ‘Great Unconformity’ and kick-started the modern active phase of plate tectonics: Stephan Sobolev and Michael Brown, "Surface erosion events controlled the evolution of plate tectonics on Earth”. Nature 570, 52-57 DOI: 10.1038/s41586-019-1258-4
November 2018 - Our article in Nature Geoscience explains how about 60 million years ago simultaneous widspread volcanism could occur in the North Atlantic and west of Greenland. It also explains a corridor of thinned lithosphere across Greenland: Bernhard Steinberger, Eva Bredow, Sergei Lebedev, Andrew Schaeffer, Trond H. Torsvik (2018) "Widespread volcanism in the Greenland-North Atlantic region explained by the Iceland plume". Nature Geoscience, 10.1038/s41561-018-0251-0
February 2018 - Eva Bredow was honored with the Günter-Bock-Preis from DGG in recognation of her publication "How plume-ridge interaction shapes the crustal thickness pattern of the Réunion hotspot track".
Subduction is a key process of Plate Tectonics. We develop thermomechanical models of subduction in a large range of temporal scales, from minutes (earthquake) to seismic cycle of great earthquake (centuries) and multiple seismic cycles (millennia), to long term evolution over the millions of years. We study initiation of subduction in early Earth and in present day settings including passive margins and oceanic basins. We also model effect of subduction on deformation of the overriding plate with a type example of South American Andes.
Webpage of working group Subduction across the Scales
The Earth's mantle behaves like a very viscous liquid over extended geological periods. Cold earth plates sink from the surface to the core-mantle boundary, and hot material rises from there in the form of mantle plumes and as large-scale upwellings. By numerical modeling with different observation data, in particular from seismology, geodesy and mineral physics as boundary conditions, we try to better understand processes in the Earth's interior. In particular, we investigate the following topics:
Webpage of working group Mantle convection and plate tectonics
Continental rifting occurs where Earth’s plates are stretched like in the East African Rift System. During break-up two passive rifted margins are formed straddling a new ocean basin. We investigate the dynamics of continental rifts and passive margins by combining numerical simulations with geophysical and geological observations. To this aim we model processes that range from mantle convection and plumes over lithosphere deformation at plate boundaries to strain localization on the cm-scale.
Webpage of working group CRYSTALS
Since the Great Sumatra 2004 Boxing Day earthquake and tsunami GFZ provides research and methodologic development in the fields of tsunami hazard assessment and early warning. Section 2.5 Geodynamic Modeling supports these activities with numerical modeling of tsunami generation, propagation and coastal impact within both deterministic and probabilistic frameworks. Our Section also participates in the development of the innovative GNSS-based technology for tsunami early warning.
Webpage of Tsunami Hazard Assessment and Early Warning