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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ftdatacite:10.15488/15466 2023-12-31T10:07:59+01:00 Deformation of salt structures by ice-sheet loading: insights into the controlling parameters from numerical modelling ... Lang, Jörg Hampel, Andrea 2023 https://dx.doi.org/10.15488/15466 https://www.repo.uni-hannover.de/handle/123456789/15587 en eng Berlin Heidelberg : Springer Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Finite-element modelling ABAQUS Glaciation Ice-sheet loading Salt mechanics Salt structures Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften ScholarlyArticle Text article-journal Article 2023 ftdatacite https://doi.org/10.15488/15466 2023-12-01T11:30:46Z 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 ... Text Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Finite-element modelling ABAQUS Glaciation Ice-sheet loading Salt mechanics Salt structures Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften |
spellingShingle |
Finite-element modelling ABAQUS Glaciation Ice-sheet loading Salt mechanics Salt structures Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften 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 Dewey Decimal Classification500 | Naturwissenschaften550 | Geowissenschaften |
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 ... |
format |
Text |
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://dx.doi.org/10.15488/15466 https://www.repo.uni-hannover.de/handle/123456789/15587 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.15488/15466 |
_version_ |
1786840535221141504 |