Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ...
Strong compressive and shear stresses generated by glacial loading and unloading have a direct impact on near-surface geological processes. Glacial stresses are constantly evolving, creating stress perturbations in the lithosphere that extend significant distances away from the ice load. In the Arct...
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ftdatacite:10.18710/qbsweh 2023-11-05T03:38:44+01:00 Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... Vachon, Rémi 2022 https://dx.doi.org/10.18710/qbsweh https://dataverse.no/citation?persistentId=doi:10.18710/QBSWEH unknown DataverseNO https://dx.doi.org/10.18710/qbsweh/a3ee3a https://dx.doi.org/10.18710/qbsweh/n89vov https://dx.doi.org/10.18710/qbsweh/d4ajaz https://dx.doi.org/10.18710/qbsweh/fjr0yn https://dx.doi.org/10.18710/qbsweh/bgpnqw https://dx.doi.org/10.18710/qbsweh/udtx4v https://dx.doi.org/10.18710/qbsweh/naf4bs https://dx.doi.org/10.18710/qbsweh/oc4ygi https://dx.doi.org/10.18710/qbsweh/9am4zj https://dx.doi.org/10.18710/qbsweh/ex4gym https://dx.doi.org/10.18710/qbsweh/qqiedz https://dx.doi.org/10.18710/qbsweh/rqn6ww https://dx.doi.org/10.18710/qbsweh/4pym3u https://dx.doi.org/10.18710/qbsweh/rkx9za https://dx.doi.org/10.18710/qbsweh/aa1iht https://dx.doi.org/10.18710/qbsweh/hb4pvi https://dx.doi.org/10.18710/qbsweh/z9xv7x https://dx.doi.org/10.18710/qbsweh/iv67oz https://dx.doi.org/10.18710/qbsweh/qmjtnq https://dx.doi.org/10.18710/qbsweh/cceavg Dataset dataset 2022 ftdatacite https://doi.org/10.18710/qbsweh10.18710/qbsweh/a3ee3a10.18710/qbsweh/n89vov10.18710/qbsweh/d4ajaz10.18710/qbsweh/fjr0yn10.18710/qbsweh/bgpnqw10.18710/qbsweh/udtx4v10.18710/qbsweh/naf4bs10.18710/qbsweh/oc4ygi10.18710/qbsweh/9am4zj10.18710/qbsweh/ex4gym10.1 2023-10-09T11:09:16Z Strong compressive and shear stresses generated by glacial loading and unloading have a direct impact on near-surface geological processes. Glacial stresses are constantly evolving, creating stress perturbations in the lithosphere that extend significant distances away from the ice load. In the Arctic, periodic methane seepage and faulting have been recurrently associated with glacial cycles. However, the evolution of the Arctic glacial stress field and its impact on the upper lithosphere have not been investigated. Here, we compute the evolution in space and time of the glacial stresses induced in the Arctic lithosphere by the North American, Eurasian and Greenland ice sheets during the latest glaciation. We use glacial isostatic adjustment (GIA) methodology to investigate the response of spherical, viscoelastic Earth models with varying lithospheric thickness to the ice loads. The magnitude of the vertical GIA-related stress closely follows the changing ice thickness, whilst the horizontal stresses are ... Dataset Arctic Greenland 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 |
unknown |
description |
Strong compressive and shear stresses generated by glacial loading and unloading have a direct impact on near-surface geological processes. Glacial stresses are constantly evolving, creating stress perturbations in the lithosphere that extend significant distances away from the ice load. In the Arctic, periodic methane seepage and faulting have been recurrently associated with glacial cycles. However, the evolution of the Arctic glacial stress field and its impact on the upper lithosphere have not been investigated. Here, we compute the evolution in space and time of the glacial stresses induced in the Arctic lithosphere by the North American, Eurasian and Greenland ice sheets during the latest glaciation. We use glacial isostatic adjustment (GIA) methodology to investigate the response of spherical, viscoelastic Earth models with varying lithospheric thickness to the ice loads. The magnitude of the vertical GIA-related stress closely follows the changing ice thickness, whilst the horizontal stresses are ... |
format |
Dataset |
author |
Vachon, Rémi |
spellingShingle |
Vachon, Rémi Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
author_facet |
Vachon, Rémi |
author_sort |
Vachon, Rémi |
title |
Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
title_short |
Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
title_full |
Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
title_fullStr |
Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
title_full_unstemmed |
Stresses, vertical displacement and velocities for model TE60, TE120 and VL20-175 at the LGM (23kyrsBP) and present ... |
title_sort |
stresses, vertical displacement and velocities for model te60, te120 and vl20-175 at the lgm (23kyrsbp) and present ... |
publisher |
DataverseNO |
publishDate |
2022 |
url |
https://dx.doi.org/10.18710/qbsweh https://dataverse.no/citation?persistentId=doi:10.18710/QBSWEH |
genre |
Arctic Greenland |
genre_facet |
Arctic Greenland |
op_relation |
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op_doi |
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