Seafloor craters and mounds in the central Barents Sea

Multiple giant craters and mounds have been identified in the area of the Upper Bjørnøyrenna in the central Barents Sea from the reflection seismic and echo sounder data. Analysis of seismic and echo sounder data revealed clear connection between these distinct seafloor features and seismic amplitud...

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Bibliographic Details
Main Author: Isaksen, Nataliia
Format: Master Thesis
Language:English
Published: UiT The Arctic University of Norway 2016
Subjects:
Online Access:https://hdl.handle.net/10037/11089
id ftunivtroemsoe:oai:munin.uit.no:10037/11089
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/11089 2023-05-15T15:38:28+02:00 Seafloor craters and mounds in the central Barents Sea Isaksen, Nataliia 2016-05-31 https://hdl.handle.net/10037/11089 eng eng UiT The Arctic University of Norway UiT Norges arktiske universitet https://hdl.handle.net/10037/11089 openAccess Copyright 2016 The Author(s) VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 gas leakage gas hydrate the central Barents Sea the Bjørnøyrenna Late Weichselian Maximum collapsed gas hydrate pingoes collapsed depressions giant craters VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456 EOM-3901 Master thesis Mastergradsoppgave 2016 ftunivtroemsoe 2021-06-25T17:55:17Z Multiple giant craters and mounds have been identified in the area of the Upper Bjørnøyrenna in the central Barents Sea from the reflection seismic and echo sounder data. Analysis of seismic and echo sounder data revealed clear connection between these distinct seafloor features and seismic amplitude anomalies. Distribution pattern of the numerous water column anomalies registered in the area and interpreted to be gas plumes, corresponds to the location of faults in the study area what suggest that gas is of thermogenic origin and is migrating from the deeper reservoir through porous layers and faults working as vertical conduits. Suggested that craters and mounds are collapsed depressions and collapsed gas hydrate pingoes and their formation is associated with the processes of formation and decomposition of shallow gas hydrates due to the last glaciation period in the area, the Late Weichselian Maximum. 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 leakage
gas hydrate
the central Barents Sea
the Bjørnøyrenna
Late Weichselian Maximum
collapsed gas hydrate pingoes
collapsed depressions
giant craters
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456
EOM-3901
spellingShingle VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
gas leakage
gas hydrate
the central Barents Sea
the Bjørnøyrenna
Late Weichselian Maximum
collapsed gas hydrate pingoes
collapsed depressions
giant craters
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456
EOM-3901
Isaksen, Nataliia
Seafloor craters and mounds in the central Barents Sea
topic_facet VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
gas leakage
gas hydrate
the central Barents Sea
the Bjørnøyrenna
Late Weichselian Maximum
collapsed gas hydrate pingoes
collapsed depressions
giant craters
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456
EOM-3901
description Multiple giant craters and mounds have been identified in the area of the Upper Bjørnøyrenna in the central Barents Sea from the reflection seismic and echo sounder data. Analysis of seismic and echo sounder data revealed clear connection between these distinct seafloor features and seismic amplitude anomalies. Distribution pattern of the numerous water column anomalies registered in the area and interpreted to be gas plumes, corresponds to the location of faults in the study area what suggest that gas is of thermogenic origin and is migrating from the deeper reservoir through porous layers and faults working as vertical conduits. Suggested that craters and mounds are collapsed depressions and collapsed gas hydrate pingoes and their formation is associated with the processes of formation and decomposition of shallow gas hydrates due to the last glaciation period in the area, the Late Weichselian Maximum.
format Master Thesis
author Isaksen, Nataliia
author_facet Isaksen, Nataliia
author_sort Isaksen, Nataliia
title Seafloor craters and mounds in the central Barents Sea
title_short Seafloor craters and mounds in the central Barents Sea
title_full Seafloor craters and mounds in the central Barents Sea
title_fullStr Seafloor craters and mounds in the central Barents Sea
title_full_unstemmed Seafloor craters and mounds in the central Barents Sea
title_sort seafloor craters and mounds in the central barents sea
publisher UiT The Arctic University of Norway
publishDate 2016
url https://hdl.handle.net/10037/11089
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_relation https://hdl.handle.net/10037/11089
op_rights openAccess
Copyright 2016 The Author(s)
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