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: Text
Language:English
Published: Berlin 2023
Subjects:
Online Access:https://dx.doi.org/10.15488/15466
https://www.repo.uni-hannover.de/handle/123456789/15587
id ftdatacite:10.15488/15466
record_format openpolar
spelling 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)
institution 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
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