Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait
Source at https://doi.org/10.1002/2014GL062474 . An edited version of this paper was published by AGU. Copyright 2015 American Geophysical Union. Methane expulsion from the world ocean floor is a broadly observed phenomenon known to be episodic. Yet the processes that modulate seepage remain elusive...
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Online Access: | https://hdl.handle.net/10037/13857 https://doi.org/10.1002/2014GL062474 |
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ftunivtroemsoe:oai:munin.uit.no:10037/13857 2023-05-15T14:27:18+02:00 Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait Plaza-Faverola, Andreia Bünz, Stefan Johnson, Joel E Chand, Shyam Knies, Jochen Mienert, Jurgen Franek, Peter 2015-01-13 https://hdl.handle.net/10037/13857 https://doi.org/10.1002/2014GL062474 eng eng American Geophysical Union (AGU) Geophysical Research Letters info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ Plaza-Faverola, A., Bünz, S., Johnson, J.E., Chand, S., Knies, J., Mienert, J. & Franek, P. (2015). Role of tectonic stress in seepage evolution along the gas hydrate-charged Vestnesa Ridge, Fram Strait. Geophysical Research Letters. 42(3), 733-742. https://doi.org/10.1002/2014GL062474 FRIDAID 1229758 doi:10.1002/2014GL062474 0094-8276 1944-8007 https://hdl.handle.net/10037/13857 openAccess VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 3-D seismic hydrates methane seepage tectonic stress Vestnesa Ridge Arctic Journal article Tidsskriftartikkel Peer reviewed 2015 ftunivtroemsoe https://doi.org/10.1002/2014GL062474 2021-06-25T17:55:44Z Source at https://doi.org/10.1002/2014GL062474 . An edited version of this paper was published by AGU. Copyright 2015 American Geophysical Union. Methane expulsion from the world ocean floor is a broadly observed phenomenon known to be episodic. Yet the processes that modulate seepage remain elusive. In the Arctic offshore west Svalbard, for instance, seepage at 200–400 m water depth may be explained by ocean temperature‐controlled gas hydrate instabilities at the shelf break, but additional processes are required to explain seepage in permanently cold waters at depths >1000 m. We discuss the influence of tectonic stress on seepage evolution along the ~100 km long hydrate‐bearing Vestnesa Ridge in Fram Strait. High‐resolution P‐Cable 3‐D seismic data revealed fine‐scale (>10 m width) near‐vertical faults and fractures controlling seepage distribution. Gas chimneys record multiple seepage events coinciding with glacial intensification and active faulting. The faults document the influence of nearby tectonic stress fields in seepage evolution along this deepwater gas hydrate system for at least the last ~2.7 Ma. Article in Journal/Newspaper Arctic Arctic Fram Strait Svalbard University of Tromsø: Munin Open Research Archive Arctic Svalbard Geophysical Research Letters 42 3 733 742 |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 3-D seismic hydrates methane seepage tectonic stress Vestnesa Ridge Arctic |
spellingShingle |
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 3-D seismic hydrates methane seepage tectonic stress Vestnesa Ridge Arctic Plaza-Faverola, Andreia Bünz, Stefan Johnson, Joel E Chand, Shyam Knies, Jochen Mienert, Jurgen Franek, Peter Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
topic_facet |
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 3-D seismic hydrates methane seepage tectonic stress Vestnesa Ridge Arctic |
description |
Source at https://doi.org/10.1002/2014GL062474 . An edited version of this paper was published by AGU. Copyright 2015 American Geophysical Union. Methane expulsion from the world ocean floor is a broadly observed phenomenon known to be episodic. Yet the processes that modulate seepage remain elusive. In the Arctic offshore west Svalbard, for instance, seepage at 200–400 m water depth may be explained by ocean temperature‐controlled gas hydrate instabilities at the shelf break, but additional processes are required to explain seepage in permanently cold waters at depths >1000 m. We discuss the influence of tectonic stress on seepage evolution along the ~100 km long hydrate‐bearing Vestnesa Ridge in Fram Strait. High‐resolution P‐Cable 3‐D seismic data revealed fine‐scale (>10 m width) near‐vertical faults and fractures controlling seepage distribution. Gas chimneys record multiple seepage events coinciding with glacial intensification and active faulting. The faults document the influence of nearby tectonic stress fields in seepage evolution along this deepwater gas hydrate system for at least the last ~2.7 Ma. |
format |
Article in Journal/Newspaper |
author |
Plaza-Faverola, Andreia Bünz, Stefan Johnson, Joel E Chand, Shyam Knies, Jochen Mienert, Jurgen Franek, Peter |
author_facet |
Plaza-Faverola, Andreia Bünz, Stefan Johnson, Joel E Chand, Shyam Knies, Jochen Mienert, Jurgen Franek, Peter |
author_sort |
Plaza-Faverola, Andreia |
title |
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
title_short |
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
title_full |
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
title_fullStr |
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
title_full_unstemmed |
Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait |
title_sort |
role of tectonic stress in seepage evolution along the gas hydrate‐charged vestnesa ridge, fram strait |
publisher |
American Geophysical Union (AGU) |
publishDate |
2015 |
url |
https://hdl.handle.net/10037/13857 https://doi.org/10.1002/2014GL062474 |
geographic |
Arctic Svalbard |
geographic_facet |
Arctic Svalbard |
genre |
Arctic Arctic Fram Strait Svalbard |
genre_facet |
Arctic Arctic Fram Strait Svalbard |
op_relation |
Geophysical Research Letters info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ Plaza-Faverola, A., Bünz, S., Johnson, J.E., Chand, S., Knies, J., Mienert, J. & Franek, P. (2015). Role of tectonic stress in seepage evolution along the gas hydrate-charged Vestnesa Ridge, Fram Strait. Geophysical Research Letters. 42(3), 733-742. https://doi.org/10.1002/2014GL062474 FRIDAID 1229758 doi:10.1002/2014GL062474 0094-8276 1944-8007 https://hdl.handle.net/10037/13857 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.1002/2014GL062474 |
container_title |
Geophysical Research Letters |
container_volume |
42 |
container_issue |
3 |
container_start_page |
733 |
op_container_end_page |
742 |
_version_ |
1766300989086760960 |