Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin
Methane seepage occurs across the western Svalbard margin at water depths ranging from < 300 m, landward from the shelf break, to > 1000 m in regions just a few kilometres from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary...
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Copernicus Publications
2019
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00003562 2023-05-15T16:18:08+02:00 Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin Plaza-Faverola, Andreia Keiding, Marie 2019-01 electronic https://doi.org/10.5194/se-10-79-2019 https://noa.gwlb.de/receive/cop_mods_00003562 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003520/se-10-79-2019.pdf https://se.copernicus.org/articles/10/79/2019/se-10-79-2019.pdf eng eng Copernicus Publications Solid Earth -- 1869-9529 https://doi.org/10.5194/se-10-79-2019 https://noa.gwlb.de/receive/cop_mods_00003562 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003520/se-10-79-2019.pdf https://se.copernicus.org/articles/10/79/2019/se-10-79-2019.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2019 ftnonlinearchiv https://doi.org/10.5194/se-10-79-2019 2022-02-08T23:00:33Z Methane seepage occurs across the western Svalbard margin at water depths ranging from < 300 m, landward from the shelf break, to > 1000 m in regions just a few kilometres from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary ridge, located on oceanic crust at a depth of 1000–1700 m, hosts a perennial gas hydrate and associated free gas system. The restriction of the occurrence of acoustic flares to the eastern segment of the sedimentary ridge, despite the presence of pockmarks along the entire ridge, indicates a spatial variation in seepage activity. This variation coincides with a change in the faulting pattern as well as in the characteristics of the fluid flow features. Due to the position of the Vestnesa Ridge with respect to the Molloy and Knipovich mid-ocean ridges, it has been suggested that seepage along the ridge has a tectonic control. We modelled the tectonic stress regime due to oblique spreading along the Molloy and Knipovich ridges to investigate whether spatial variations in the tectonic regime along the Vestnesa Ridge are plausible. The model predicts a zone of tensile stress that extends northward from the Knipovich Ridge and encompasses the zone of acoustic flares on the eastern Vestnesa Ridge. In this zone the orientation of the maximum principal stress is parallel to pre-existing faults. The model predicts a strike-slip stress regime in regions with pockmarks where acoustic flares have not been documented. If a certain degree of coupling is assumed between deep crustal and near-surface deformation, it is possible that ridge-push forces have influenced seepage activity in the region by interacting with the pore-pressure regime at the base of the gas hydrate stability zone. More abundant seepage on the eastern Vestnesa Ridge at present may be facilitated by the dilation of faults and fractures favourably oriented with respect to the stress field. A modified state of stress in the past, due to more significant glacial stress for instance, may explain vigorous seepage activity along the entire Vestnesa Ridge. The contribution of other mechanisms to the state of stress (i.e. sedimentary loading and lithospheric flexure) remain to be investigated. Our study provides a first-order assessment of how tectonic stresses may be influencing the kinematics of near-surface faults and associated seepage activity offshore of the western Svalbard margin. Article in Journal/Newspaper Fram Strait Svalbard Svalbard margin Niedersächsisches Online-Archiv NOA Knipovich Ridge ENVELOPE(7.074,7.074,75.712,75.712) Molloy ENVELOPE(70.065,70.065,-49.360,-49.360) Svalbard Solid Earth 10 1 79 94 |
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Open Polar |
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Niedersächsisches Online-Archiv NOA |
op_collection_id |
ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
spellingShingle |
article Verlagsveröffentlichung Plaza-Faverola, Andreia Keiding, Marie Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
topic_facet |
article Verlagsveröffentlichung |
description |
Methane seepage occurs across the western Svalbard margin at water depths ranging from < 300 m, landward from the shelf break, to > 1000 m in regions just a few kilometres from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary ridge, located on oceanic crust at a depth of 1000–1700 m, hosts a perennial gas hydrate and associated free gas system. The restriction of the occurrence of acoustic flares to the eastern segment of the sedimentary ridge, despite the presence of pockmarks along the entire ridge, indicates a spatial variation in seepage activity. This variation coincides with a change in the faulting pattern as well as in the characteristics of the fluid flow features. Due to the position of the Vestnesa Ridge with respect to the Molloy and Knipovich mid-ocean ridges, it has been suggested that seepage along the ridge has a tectonic control. We modelled the tectonic stress regime due to oblique spreading along the Molloy and Knipovich ridges to investigate whether spatial variations in the tectonic regime along the Vestnesa Ridge are plausible. The model predicts a zone of tensile stress that extends northward from the Knipovich Ridge and encompasses the zone of acoustic flares on the eastern Vestnesa Ridge. In this zone the orientation of the maximum principal stress is parallel to pre-existing faults. The model predicts a strike-slip stress regime in regions with pockmarks where acoustic flares have not been documented. If a certain degree of coupling is assumed between deep crustal and near-surface deformation, it is possible that ridge-push forces have influenced seepage activity in the region by interacting with the pore-pressure regime at the base of the gas hydrate stability zone. More abundant seepage on the eastern Vestnesa Ridge at present may be facilitated by the dilation of faults and fractures favourably oriented with respect to the stress field. A modified state of stress in the past, due to more significant glacial stress for instance, may explain vigorous seepage activity along the entire Vestnesa Ridge. The contribution of other mechanisms to the state of stress (i.e. sedimentary loading and lithospheric flexure) remain to be investigated. Our study provides a first-order assessment of how tectonic stresses may be influencing the kinematics of near-surface faults and associated seepage activity offshore of the western Svalbard margin. |
format |
Article in Journal/Newspaper |
author |
Plaza-Faverola, Andreia Keiding, Marie |
author_facet |
Plaza-Faverola, Andreia Keiding, Marie |
author_sort |
Plaza-Faverola, Andreia |
title |
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
title_short |
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
title_full |
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
title_fullStr |
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
title_full_unstemmed |
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin |
title_sort |
correlation between tectonic stress regimes and methane seepage on the western svalbard margin |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/se-10-79-2019 https://noa.gwlb.de/receive/cop_mods_00003562 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003520/se-10-79-2019.pdf https://se.copernicus.org/articles/10/79/2019/se-10-79-2019.pdf |
long_lat |
ENVELOPE(7.074,7.074,75.712,75.712) ENVELOPE(70.065,70.065,-49.360,-49.360) |
geographic |
Knipovich Ridge Molloy Svalbard |
geographic_facet |
Knipovich Ridge Molloy Svalbard |
genre |
Fram Strait Svalbard Svalbard margin |
genre_facet |
Fram Strait Svalbard Svalbard margin |
op_relation |
Solid Earth -- 1869-9529 https://doi.org/10.5194/se-10-79-2019 https://noa.gwlb.de/receive/cop_mods_00003562 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003520/se-10-79-2019.pdf https://se.copernicus.org/articles/10/79/2019/se-10-79-2019.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/se-10-79-2019 |
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Solid Earth |
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10 |
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container_start_page |
79 |
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