Articles | Volume 12, issue 8
https://doi.org/10.5194/se-12-1777-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-1777-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Aug 2021
Research article |
| 11 Aug 2021
3D crustal stress state of Germany according to a data-calibrated geomechanical model
Steffen Ahlers
CORRESPONDING AUTHOR
Engineering Geology, Institute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, Germany
Andreas Henk
Engineering Geology, Institute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, Germany
Tobias Hergert
Engineering Geology, Institute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, Germany
Karsten Reiter
Engineering Geology, Institute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, Germany
Birgit Müller
Technical Petrophysics, Institute of Applied Geosciences, KIT, 76131 Karlsruhe, Germany
Luisa Röckel
Technical Petrophysics, Institute of Applied Geosciences, KIT, 76131 Karlsruhe, Germany
Oliver Heidbach
Seismic Hazard and Risk Dynamics, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Institute for Applied Geosciences, TU Berlin, 10587 Berlin, Germany
Sophia Morawietz
Seismic Hazard and Risk Dynamics, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Institute for Applied Geosciences, TU Berlin, 10587 Berlin, Germany
Magdalena Scheck-Wenderoth
Basin Modelling, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Department of Geology, Geochemistry of Petroleum and Coal, Faculty of Georesources and Material Engineering, RWTH Aachen University, Aachen, Germany
Denis Anikiev
Basin Modelling, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
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Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
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K. Reiter and O. Heidbach
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Y. Cherubini, M. Cacace, M. Scheck-Wenderoth, and V. Noack
Geoth. Energ. Sci., 2, 1–20, https://doi.org/10.5194/gtes-2-1-2014, https://doi.org/10.5194/gtes-2-1-2014, 2014
K. Fischer and A. Henk
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Related subject area
Subject area: Tectonic plate interactions, magma genesis, and lithosphere deformation at all scales | Editorial team: Geodynamics and quantitative modelling | Discipline: Tectonics
Tectonic interactions during rift linkage: insights from analog and numerical experiments
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Anthony Jourdon and Dave A. May
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Sepideh Pajang, Laetitia Le Pourhiet, and Nadaya Cubas
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Anthony Jourdon, Charlie Kergaravat, Guillaume Duclaux, and Caroline Huguen
Solid Earth, 12, 1211–1232, https://doi.org/10.5194/se-12-1211-2021, https://doi.org/10.5194/se-12-1211-2021, 2021
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The borders between oceans and continents, called margins, can be convergent, divergent, or horizontally sliding. The formation of oceans occurs in a divergent context. However, some divergent margin structures display an accommodation of horizontal sliding during the opening of oceans. To study and understand how the horizontal sliding part occurring during divergence influences the margin structure, we performed 3D high-resolution numerical models evolving during tens of millions of years.
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Short summary
Knowledge about the stress state in the upper crust is of great importance for many economic and scientific questions. However, our knowledge in Germany is limited since available datasets only provide pointwise, incomplete and heterogeneous information. We present the first 3D geomechanical model that provides a continuous description of the contemporary crustal stress state for Germany. The model is calibrated by the orientation of the maximum horizontal stress and stress magnitudes.
Knowledge about the stress state in the upper crust is of great importance for many economic and...
