Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling

Subsurface salt flow is driven by differential loading, which is typically caused by tectonics or sedimentation. During glaciations, the weight of an ice sheet represents another source of differential loading. In salt-bearing basins affected by Pleistocene glaciations, such as the Central European...

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Main Authors: Lang, Jörg, Hampel, Andrea
Format: Article in Journal/Newspaper
Language:English
Published: Berlin 2023
Subjects:
Online Access:https://www.repo.uni-hannover.de/handle/123456789/15587
https://doi.org/10.15488/15466
id ftunivhannover:oai:www.repo.uni-hannover.de:123456789/15587
record_format openpolar
spelling ftunivhannover:oai:www.repo.uni-hannover.de:123456789/15587 2023-12-24T10:17:35+01:00 Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling Lang, Jörg Hampel, Andrea 2023 https://www.repo.uni-hannover.de/handle/123456789/15587 https://doi.org/10.15488/15466 eng eng Berlin Heidelberg : Springer DOI:https://doi.org/10.1007/s00531-023-02295-5 ISSN:1437-3254 ESSN:1437-3262 http://dx.doi.org/10.15488/15466 https://www.repo.uni-hannover.de/handle/123456789/15587 CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0 frei zugänglich International Journal of Earth Sciences 112 (2023), Nr. 4 International Journal of Earth Sciences Finite-element modelling (ABAQUS) Glaciation Ice-sheet loading Salt mechanics Salt structures ddc:550 status-type:publishedVersion doc-type:Article doc-type:Text 2023 ftunivhannover https://doi.org/10.15488/1546610.1007/s00531-023-02295-5 2023-11-26T23:47:00Z Subsurface salt flow is driven by differential loading, which is typically caused by tectonics or sedimentation. During glaciations, the weight of an ice sheet represents another source of differential loading. In salt-bearing basins affected by Pleistocene glaciations, such as the Central European Basin System, ice loading has been postulated as a trigger of young deformation at salt structures. Here, we present finite-element simulations (ABAQUS) with models based on a simplified 50-km long and 10-km-deep two-dimensional geological cross-section of a salt diapir subject to the load of a 300-m-thick ice sheet. The focus of our study is to evaluate the sensitivity of the model to material parameters, including linear and non-linear viscosity of the salt rocks and different elasticities. A spatially and temporarily variable pressure was applied to simulate ice loading. An ice advance towards the diapir causes lateral salt flow into the diapir and diapiric rise. Complete ice coverage leads to downward displacement of the diapir. After unloading, displacements are largely restored. The modelled displacements do not exceed few metres and are always larger in models with linear viscosity than in those with non-linear viscosity. Considering the low stresses caused by ice-sheet loading and the long time-scale, the application of linear viscosity seems appropriate. The elastic parameters also have a strong impact, with lower Young's moduli leading to larger deformation. The impact of both the viscosity and the elasticity highlights the importance of a careful parameter choice in numerical modelling, especially when aiming to replicate any real-world observations. Article in Journal/Newspaper Ice Sheet Institutional Repository of Leibniz Universität Hannover
institution Open Polar
collection Institutional Repository of Leibniz Universität Hannover
op_collection_id ftunivhannover
language English
topic Finite-element modelling (ABAQUS)
Glaciation
Ice-sheet loading
Salt mechanics
Salt structures
ddc:550
spellingShingle Finite-element modelling (ABAQUS)
Glaciation
Ice-sheet loading
Salt mechanics
Salt structures
ddc:550
Lang, Jörg
Hampel, Andrea
Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
topic_facet Finite-element modelling (ABAQUS)
Glaciation
Ice-sheet loading
Salt mechanics
Salt structures
ddc:550
description Subsurface salt flow is driven by differential loading, which is typically caused by tectonics or sedimentation. During glaciations, the weight of an ice sheet represents another source of differential loading. In salt-bearing basins affected by Pleistocene glaciations, such as the Central European Basin System, ice loading has been postulated as a trigger of young deformation at salt structures. Here, we present finite-element simulations (ABAQUS) with models based on a simplified 50-km long and 10-km-deep two-dimensional geological cross-section of a salt diapir subject to the load of a 300-m-thick ice sheet. The focus of our study is to evaluate the sensitivity of the model to material parameters, including linear and non-linear viscosity of the salt rocks and different elasticities. A spatially and temporarily variable pressure was applied to simulate ice loading. An ice advance towards the diapir causes lateral salt flow into the diapir and diapiric rise. Complete ice coverage leads to downward displacement of the diapir. After unloading, displacements are largely restored. The modelled displacements do not exceed few metres and are always larger in models with linear viscosity than in those with non-linear viscosity. Considering the low stresses caused by ice-sheet loading and the long time-scale, the application of linear viscosity seems appropriate. The elastic parameters also have a strong impact, with lower Young's moduli leading to larger deformation. The impact of both the viscosity and the elasticity highlights the importance of a careful parameter choice in numerical modelling, especially when aiming to replicate any real-world observations.
format Article in Journal/Newspaper
author Lang, Jörg
Hampel, Andrea
author_facet Lang, Jörg
Hampel, Andrea
author_sort Lang, Jörg
title Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
title_short Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
title_full Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
title_fullStr Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
title_full_unstemmed Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
title_sort deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling
publisher Berlin
publishDate 2023
url https://www.repo.uni-hannover.de/handle/123456789/15587
https://doi.org/10.15488/15466
genre Ice Sheet
genre_facet Ice Sheet
op_source International Journal of Earth Sciences 112 (2023), Nr. 4
International Journal of Earth Sciences
op_relation DOI:https://doi.org/10.1007/s00531-023-02295-5
ISSN:1437-3254
ESSN:1437-3262
http://dx.doi.org/10.15488/15466
https://www.repo.uni-hannover.de/handle/123456789/15587
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0
frei zugänglich
op_doi https://doi.org/10.15488/1546610.1007/s00531-023-02295-5
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