Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt

Abstract In foreland fold-and-thrust belts, the distribution of deformation and of the associated stress field can notably be perturbed due to local-scale features such as tectonic structures or surface topography. In the context of geothermal exploration and the planning of the future circular coll...

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Main Authors: Sandra Borderie, Jon Mosar, Adeline Marro, Louis Hauvette
Format: Article
Language:English
Published: SpringerOpen 2025-06-01
Series:Swiss Journal of Geosciences
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Online Access:https://doi.org/10.1186/s00015-025-00483-w
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author Sandra Borderie
Jon Mosar
Adeline Marro
Louis Hauvette
author_facet Sandra Borderie
Jon Mosar
Adeline Marro
Louis Hauvette
author_sort Sandra Borderie
collection DOAJ
description Abstract In foreland fold-and-thrust belts, the distribution of deformation and of the associated stress field can notably be perturbed due to local-scale features such as tectonic structures or surface topography. In the context of geothermal exploration and the planning of the future circular collider (CERN) in the Geneva Basin, it is of particular interest to constrain possible future deformation in the area and the associated stress state. If current seismicity indicates that the Geneva Basin is tectonically active, few data regarding the state of stress in the area are currently available. The goal of this study is to understand under which conditions deformation could localise in the study area, by using numerical modelling based on Limit Analysis. In a first regional part of the study, we investigate the impact of the basal décollement strength on the deformation and on the stress field along a 2D section. Knowing the weak décollement property in the area, results indicate that future deformation is more likely to localise in the Geneva Basin or at the frontal part of the Jura fold-and-thrust belt. Location of deformation in the Geneva Basin depends more on surface topography rather than on décollement geometry. The décollement geometry influences the presence of stress concentrations, which could lead to weakness zones within the section. In the second part of the study, we used a simplified prototype section based on interpretation of a seismic surveys in the Geneva Basin. The impact of the inherited faults strength on incipient deformation was investigated. Results indicate that existing faults can be reactivated by decreasing their friction angle. In the Geneva Basin, the Humilly Fault is the less likely to be reactivated, due to its orientation, compared to the Reculet and Salève thrusts. The failure potential is thus strongly determined by the internal structure of the considered prototype, the frictional properties, and orientations of the existing faults. In the case where deformation localises in the Geneva Basin, the differential stress distribution depends on the décollement strength and geometry, and of the strength of the existing faults.
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spelling doaj-art-a5cc4085245f46bcad5d4f73099d57192025-08-20T02:30:43ZengSpringerOpenSwiss Journal of Geosciences1661-87261661-87342025-06-01118112410.1186/s00015-025-00483-wUnlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust beltSandra Borderie0Jon Mosar1Adeline Marro2Louis Hauvette3Earth Sciences Unit, Department of Geosciences, University of FribourgEarth Sciences Unit, Department of Geosciences, University of FribourgEarth Sciences Unit, Department of Geosciences, University of FribourgEarth Sciences Unit, Department of Geosciences, University of FribourgAbstract In foreland fold-and-thrust belts, the distribution of deformation and of the associated stress field can notably be perturbed due to local-scale features such as tectonic structures or surface topography. In the context of geothermal exploration and the planning of the future circular collider (CERN) in the Geneva Basin, it is of particular interest to constrain possible future deformation in the area and the associated stress state. If current seismicity indicates that the Geneva Basin is tectonically active, few data regarding the state of stress in the area are currently available. The goal of this study is to understand under which conditions deformation could localise in the study area, by using numerical modelling based on Limit Analysis. In a first regional part of the study, we investigate the impact of the basal décollement strength on the deformation and on the stress field along a 2D section. Knowing the weak décollement property in the area, results indicate that future deformation is more likely to localise in the Geneva Basin or at the frontal part of the Jura fold-and-thrust belt. Location of deformation in the Geneva Basin depends more on surface topography rather than on décollement geometry. The décollement geometry influences the presence of stress concentrations, which could lead to weakness zones within the section. In the second part of the study, we used a simplified prototype section based on interpretation of a seismic surveys in the Geneva Basin. The impact of the inherited faults strength on incipient deformation was investigated. Results indicate that existing faults can be reactivated by decreasing their friction angle. In the Geneva Basin, the Humilly Fault is the less likely to be reactivated, due to its orientation, compared to the Reculet and Salève thrusts. The failure potential is thus strongly determined by the internal structure of the considered prototype, the frictional properties, and orientations of the existing faults. In the case where deformation localises in the Geneva Basin, the differential stress distribution depends on the décollement strength and geometry, and of the strength of the existing faults.https://doi.org/10.1186/s00015-025-00483-wGeneva BasinJura fold-and-thrust beltFold-and-thrust beltLimit analysisStressDeformation
spellingShingle Sandra Borderie
Jon Mosar
Adeline Marro
Louis Hauvette
Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
Swiss Journal of Geosciences
Geneva Basin
Jura fold-and-thrust belt
Fold-and-thrust belt
Limit analysis
Stress
Deformation
title Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
title_full Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
title_fullStr Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
title_full_unstemmed Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
title_short Unlocking the hidden forces: deformation and associated stress distribution in the present-day Geneva Basin and Jura fold-and-thrust belt
title_sort unlocking the hidden forces deformation and associated stress distribution in the present day geneva basin and jura fold and thrust belt
topic Geneva Basin
Jura fold-and-thrust belt
Fold-and-thrust belt
Limit analysis
Stress
Deformation
url https://doi.org/10.1186/s00015-025-00483-w
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