Articles | Volume 15, issue 12
https://doi.org/10.5194/se-15-1445-2024
© Author(s) 2024. 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-15-1445-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Understanding the stress field at the lateral termination of a thrust fold using generic geomechanical models and clustering methods
Anthony Adwan
CORRESPONDING AUTHOR
CY Cergy Paris Université, Laboratoire Géosciences et Environnement Cergy (GEC), 1, rue Descartes, 95000 Neuville-sur-Oise, France
now at: IRSN, Institute for Radiological Protection and Nuclear Safety, 31 Av. de la Division Leclerc, 92260 Fontenay-aux-Roses, France
Bertrand Maillot
CY Cergy Paris Université, Laboratoire Géosciences et Environnement Cergy (GEC), 1, rue Descartes, 95000 Neuville-sur-Oise, France
Pauline Souloumiac
CY Cergy Paris Université, Laboratoire Géosciences et Environnement Cergy (GEC), 1, rue Descartes, 95000 Neuville-sur-Oise, France
Christophe Barnes
CY Cergy Paris Université, Laboratoire Géosciences et Environnement Cergy (GEC), 1, rue Descartes, 95000 Neuville-sur-Oise, France
Christophe Nussbaum
Swisstopo, Federal Office of Topography, Route de la Gare 63, 2882 Saint-Ursanne, Switzerland
Meinert Rahn
Swiss Federal Nuclear Safety Inspectorate, Brugg, Switzerland
Thomas Van Stiphout
Swiss Federal Nuclear Safety Inspectorate, Brugg, Switzerland
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Jens T. Birkholzer, Yves Guglielmi, and Christophe Nussbaum
Saf. Nucl. Waste Disposal, 2, 61–62, https://doi.org/10.5194/sand-2-61-2023, https://doi.org/10.5194/sand-2-61-2023, 2023
Short summary
Short summary
This presentation discusses a series of in situ experiments of fault activation by fluid injection conducted in argillite rock at the Mont Terri underground research laboratory in Switzerland to better understand whether pressurization of natural faults can lead to their reactivation and permeability generation in case such features are present near disposal tunnels. Lessons learned from these experiments help inform the safety assessment of geologic disposal in argillite host rock.
Lisa Winhausen, Jop Klaver, Joyce Schmatz, Guillaume Desbois, Janos L. Urai, Florian Amann, and Christophe Nussbaum
Solid Earth, 12, 2109–2126, https://doi.org/10.5194/se-12-2109-2021, https://doi.org/10.5194/se-12-2109-2021, 2021
Short summary
Short summary
An experimentally deformed sample of Opalinus Clay (OPA), which is being considered as host rock for nuclear waste in Switzerland, was studied by electron microscopy to image deformation microstructures. Deformation localised by forming micrometre-thick fractures. Deformation zones show dilatant micro-cracking, granular flow and bending grains, and pore collapse. Our model, with three different stages of damage accumulation, illustrates microstructural deformation in a compressed OPA sample.
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Short summary
We use computer simulations to study how stress is distributed in large-scale geological models, focusing on how fault lines behave under pressure. By running many 2D and 3D simulations with varying conditions, we discover patterns in how faults form and interact. Our findings reveal that even small changes in conditions can lead to different stress outcomes. This research helps us better understand earthquake mechanics and could improve predictions of fault behavior in real-world scenarios.
We use computer simulations to study how stress is distributed in large-scale geological...