Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea

This Master thesis investigates the relationship between glacial erosion, glaciotectonically displaced sediment blocks and indications of fluid flow and shallow gas accumulations in buried glacial sediments of the south-western Barents Sea margin. The thesis is based on two three-dimensional (3D) se...

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Main Author: Deryabin, Alexey
Format: Master Thesis
Language:English
Published: Universitetet i Tromsø 2012
Subjects:
Online Access:https://hdl.handle.net/10037/4216
id ftunivtroemsoe:oai:munin.uit.no:10037/4216
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/4216 2023-05-15T15:38:46+02:00 Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea Deryabin, Alexey 2012-06-05 https://hdl.handle.net/10037/4216 eng eng Universitetet i Tromsø University of Tromsø https://hdl.handle.net/10037/4216 URN:NBN:no-uit_munin_3931 openAccess Copyright 2012 The Author(s) VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 Gas hydrate Craters Glacial erosion GEO-3900 Master thesis Mastergradsoppgave 2012 ftunivtroemsoe 2021-06-25T17:53:18Z This Master thesis investigates the relationship between glacial erosion, glaciotectonically displaced sediment blocks and indications of fluid flow and shallow gas accumulations in buried glacial sediments of the south-western Barents Sea margin. The thesis is based on two three-dimensional (3D) seismic datasets, NH98003 and EL0001, the two-dimensional (2D) seismic survey NH9702 and exploration well 7216/11-1. 3D seismic techniques have allowed mapping and visualizing of buried geomorphological features in great details within the study area. Large semi-circular depressions and fluid migration pathways are imaged, as well as glacigenic sediment blocks and rafts. A glacigenic origin is inferred for the megablocks and rafts indicating high glaciotectonic activity of the former ice streams. Six large-scale depressions are inferred to be sources for the removal of sediment mega-blocks and rafts at one particular stratigraphic level of the Plio-Pleistocene succession. Mapped fluid migration pathways and shallow gas accumulations show evidence of an active fluid migration system, and its spatial relationship with the erosional depressions is documented. Modeling of the gas hydrate stability zone has been performed for glacial and interglacial conditions and its effect on the sediment properties is discussed. A conceptual model is proposed for the formation of the depressions, where brittle glaciotectonic deformation along a weak layer at the base of gas-hydrate cementing sediments is inferred. Subsequent expulsion of gas-rich fluids is assumed to have followed deglaciation which might further have reworked the depressions. Master Thesis Barents Sea University of Tromsø: Munin Open Research Archive Barents Sea
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
Gas hydrate
Craters
Glacial erosion
GEO-3900
spellingShingle VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
Gas hydrate
Craters
Glacial erosion
GEO-3900
Deryabin, Alexey
Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
topic_facet VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
Gas hydrate
Craters
Glacial erosion
GEO-3900
description This Master thesis investigates the relationship between glacial erosion, glaciotectonically displaced sediment blocks and indications of fluid flow and shallow gas accumulations in buried glacial sediments of the south-western Barents Sea margin. The thesis is based on two three-dimensional (3D) seismic datasets, NH98003 and EL0001, the two-dimensional (2D) seismic survey NH9702 and exploration well 7216/11-1. 3D seismic techniques have allowed mapping and visualizing of buried geomorphological features in great details within the study area. Large semi-circular depressions and fluid migration pathways are imaged, as well as glacigenic sediment blocks and rafts. A glacigenic origin is inferred for the megablocks and rafts indicating high glaciotectonic activity of the former ice streams. Six large-scale depressions are inferred to be sources for the removal of sediment mega-blocks and rafts at one particular stratigraphic level of the Plio-Pleistocene succession. Mapped fluid migration pathways and shallow gas accumulations show evidence of an active fluid migration system, and its spatial relationship with the erosional depressions is documented. Modeling of the gas hydrate stability zone has been performed for glacial and interglacial conditions and its effect on the sediment properties is discussed. A conceptual model is proposed for the formation of the depressions, where brittle glaciotectonic deformation along a weak layer at the base of gas-hydrate cementing sediments is inferred. Subsequent expulsion of gas-rich fluids is assumed to have followed deglaciation which might further have reworked the depressions.
format Master Thesis
author Deryabin, Alexey
author_facet Deryabin, Alexey
author_sort Deryabin, Alexey
title Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
title_short Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
title_full Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
title_fullStr Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
title_full_unstemmed Relationship between glacial erosion and fluid flow inferred from 3D seismic data : SW Barents Sea
title_sort relationship between glacial erosion and fluid flow inferred from 3d seismic data : sw barents sea
publisher Universitetet i Tromsø
publishDate 2012
url https://hdl.handle.net/10037/4216
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_relation https://hdl.handle.net/10037/4216
URN:NBN:no-uit_munin_3931
op_rights openAccess
Copyright 2012 The Author(s)
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