On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...

Dissertation, RWTH Aachen University, 2023; Aachen : RWTH Aachen University 1 Online-Ressource : Illustrationen, Diagramme, Karten (2023). = Dissertation, RWTH Aachen University, 2023 ... : Physical feedback mechanisms between the subsurface and an overlying ice sheet are manifold. They lead to the...

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Main Author: Bodenburg, Sascha Barbara
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: RWTH Aachen University 2023
Subjects:
Online Access:https://dx.doi.org/10.18154/rwth-2023-09361
https://publications.rwth-aachen.de/record/969814
id ftdatacite:10.18154/rwth-2023-09361
record_format openpolar
spelling ftdatacite:10.18154/rwth-2023-09361 2024-02-27T08:41:37+00:00 On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ... Bodenburg, Sascha Barbara 2023 https://dx.doi.org/10.18154/rwth-2023-09361 https://publications.rwth-aachen.de/record/969814 en eng RWTH Aachen University Hochschulschrift tunnel valley genesis subglacial feedback mechanisms Gorleben salt dome southern North Sea apparent heat capacity methods heat conduction and hydrothermal flow Dissertation Text thesis Thesis 2023 ftdatacite https://doi.org/10.18154/rwth-2023-09361 2024-02-01T15:02:28Z Dissertation, RWTH Aachen University, 2023; Aachen : RWTH Aachen University 1 Online-Ressource : Illustrationen, Diagramme, Karten (2023). = Dissertation, RWTH Aachen University, 2023 ... : Physical feedback mechanisms between the subsurface and an overlying ice sheet are manifold. They lead to the development of special landforms, e.g. tunnel valleys. Tunnel valleys are widespread in (formerly) glaciated areas. They are eroded by subglacially flowing water. To investigate their genesis, it is necessary to model feedback mechanisms between the ice sheet and the subsurface. In the North German Basin, a possible spatial correlation between tunnel valleys and underlying salt domes was often observed. Partly, this was explained mechanically with the presence of faults. We want to investigate a different hypothesis for tunnel valley genesis based on the following geothermal argumentation: As salt better conducts heat than the surrounding rocks, the geothermal heat flux is augmented above. Hydrothermal groundwater flows through crestal faults enhance this effect. The resulting subglacial melting leads to subglacial rivers eroding the tunnel valleys. In order to determine the subglacial melting rate, ... Doctoral or Postdoctoral Thesis 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 Hochschulschrift
tunnel valley genesis
subglacial feedback mechanisms
Gorleben salt dome
southern North Sea
apparent heat capacity methods
heat conduction and hydrothermal flow
spellingShingle Hochschulschrift
tunnel valley genesis
subglacial feedback mechanisms
Gorleben salt dome
southern North Sea
apparent heat capacity methods
heat conduction and hydrothermal flow
Bodenburg, Sascha Barbara
On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
topic_facet Hochschulschrift
tunnel valley genesis
subglacial feedback mechanisms
Gorleben salt dome
southern North Sea
apparent heat capacity methods
heat conduction and hydrothermal flow
description Dissertation, RWTH Aachen University, 2023; Aachen : RWTH Aachen University 1 Online-Ressource : Illustrationen, Diagramme, Karten (2023). = Dissertation, RWTH Aachen University, 2023 ... : Physical feedback mechanisms between the subsurface and an overlying ice sheet are manifold. They lead to the development of special landforms, e.g. tunnel valleys. Tunnel valleys are widespread in (formerly) glaciated areas. They are eroded by subglacially flowing water. To investigate their genesis, it is necessary to model feedback mechanisms between the ice sheet and the subsurface. In the North German Basin, a possible spatial correlation between tunnel valleys and underlying salt domes was often observed. Partly, this was explained mechanically with the presence of faults. We want to investigate a different hypothesis for tunnel valley genesis based on the following geothermal argumentation: As salt better conducts heat than the surrounding rocks, the geothermal heat flux is augmented above. Hydrothermal groundwater flows through crestal faults enhance this effect. The resulting subglacial melting leads to subglacial rivers eroding the tunnel valleys. In order to determine the subglacial melting rate, ...
format Doctoral or Postdoctoral Thesis
author Bodenburg, Sascha Barbara
author_facet Bodenburg, Sascha Barbara
author_sort Bodenburg, Sascha Barbara
title On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
title_short On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
title_full On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
title_fullStr On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
title_full_unstemmed On the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
title_sort on the role of geothermal feedback mechanisms on tunnel valley genesis above salt domes ...
publisher RWTH Aachen University
publishDate 2023
url https://dx.doi.org/10.18154/rwth-2023-09361
https://publications.rwth-aachen.de/record/969814
genre Ice Sheet
genre_facet Ice Sheet
op_doi https://doi.org/10.18154/rwth-2023-09361
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