Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...

The attached dataset has ocean bottom seismic (OBS) data, 3D seismic data and matlab scripts used in the analysis of OBS data. OBS data was acquired using an array of 22 ocean bottom seismometers (OBS) during a research expedition (CAGE-2019-1) around Lunde pockmark, Vestnesa Ridge, W-Svalbard Margi...

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Bibliographic Details
Main Authors: Singhroha, Sunny, Plaza-Faverola, Andreia, Bünz, Stefan
Format: Dataset
Language:unknown
Published: DataverseNO 2023
Subjects:
Online Access:https://dx.doi.org/10.18710/sbr9gj
https://dataverse.no/citation?persistentId=doi:10.18710/SBR9GJ
id ftdatacite:10.18710/sbr9gj
record_format openpolar
spelling ftdatacite:10.18710/sbr9gj 2023-12-31T10:06:59+01:00 Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ... Singhroha, Sunny Plaza-Faverola, Andreia Bünz, Stefan 2023 https://dx.doi.org/10.18710/sbr9gj https://dataverse.no/citation?persistentId=doi:10.18710/SBR9GJ unknown DataverseNO https://dx.doi.org/10.18710/sbr9gj/acb01p https://dx.doi.org/10.18710/sbr9gj/qhx4ak https://dx.doi.org/10.18710/sbr9gj/1z8m26 https://dx.doi.org/10.18710/sbr9gj/jwevh0 https://dx.doi.org/10.18710/sbr9gj/q95kqv https://dx.doi.org/10.18710/sbr9gj/cixcbv https://dx.doi.org/10.18710/sbr9gj/vog7lw https://dx.doi.org/10.18710/sbr9gj/8pyecn https://dx.doi.org/10.18710/sbr9gj/jntsbv https://dx.doi.org/10.18710/sbr9gj/ba0pjg https://dx.doi.org/10.18710/sbr9gj/7bzm3t https://dx.doi.org/10.18710/sbr9gj/7giugg https://dx.doi.org/10.18710/sbr9gj/flhoni https://dx.doi.org/10.18710/sbr9gj/btr9eq https://dx.doi.org/10.18710/sbr9gj/26lxk9 https://dx.doi.org/10.18710/sbr9gj/m0llrm https://dx.doi.org/10.18710/sbr9gj/wfexpz https://dx.doi.org/10.18710/sbr9gj/xqrnjd https://dx.doi.org/10.18710/sbr9gj/vloe1i https://dx.doi.org/10.18710/sbr9gj/gbxygm Dataset dataset 2023 ftdatacite https://doi.org/10.18710/sbr9gj10.18710/sbr9gj/acb01p10.18710/sbr9gj/qhx4ak10.18710/sbr9gj/1z8m2610.18710/sbr9gj/jwevh010.18710/sbr9gj/q95kqv10.18710/sbr9gj/cixcbv10.18710/sbr9gj/vog7lw10.18710/sbr9gj/8pyecn10.18710/sbr9gj/jntsbv10.18710/sbr9gj/ba0pjg10.1 2023-12-01T10:25:59Z The attached dataset has ocean bottom seismic (OBS) data, 3D seismic data and matlab scripts used in the analysis of OBS data. OBS data was acquired using an array of 22 ocean bottom seismometers (OBS) during a research expedition (CAGE-2019-1) around Lunde pockmark, Vestnesa Ridge, W-Svalbard Margin. This data acquisition aims to improve our understanding of actively hydrocarbon gas seeping system in Vestnesa Ridge, west-Svalbard Margin. 3D seismic data was acquired in 2013 around Lunde pockmark, Vestnesa Ridge, W-Svalbard Margin using high-resolution 3D P-Cable seismic data acquisition system. Details of 3D seismic data processing and interpretation are already published in the research article "Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait" (Doi:10.1002/2014GL062474). ... Dataset Fram Strait Svalbard Svalbard margin Lunde 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 unknown
description The attached dataset has ocean bottom seismic (OBS) data, 3D seismic data and matlab scripts used in the analysis of OBS data. OBS data was acquired using an array of 22 ocean bottom seismometers (OBS) during a research expedition (CAGE-2019-1) around Lunde pockmark, Vestnesa Ridge, W-Svalbard Margin. This data acquisition aims to improve our understanding of actively hydrocarbon gas seeping system in Vestnesa Ridge, west-Svalbard Margin. 3D seismic data was acquired in 2013 around Lunde pockmark, Vestnesa Ridge, W-Svalbard Margin using high-resolution 3D P-Cable seismic data acquisition system. Details of 3D seismic data processing and interpretation are already published in the research article "Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait" (Doi:10.1002/2014GL062474). ...
format Dataset
author Singhroha, Sunny
Plaza-Faverola, Andreia
Bünz, Stefan
spellingShingle Singhroha, Sunny
Plaza-Faverola, Andreia
Bünz, Stefan
Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
author_facet Singhroha, Sunny
Plaza-Faverola, Andreia
Bünz, Stefan
author_sort Singhroha, Sunny
title Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
title_short Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
title_full Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
title_fullStr Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
title_full_unstemmed Replication data for "Stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the W-Svalbard Margin" ...
title_sort replication data for "stress constraints from shear-wave analysis in shallow sediments at an actively seeping pockmark on the w-svalbard margin" ...
publisher DataverseNO
publishDate 2023
url https://dx.doi.org/10.18710/sbr9gj
https://dataverse.no/citation?persistentId=doi:10.18710/SBR9GJ
genre Fram Strait
Svalbard
Svalbard margin
Lunde
genre_facet Fram Strait
Svalbard
Svalbard margin
Lunde
op_relation https://dx.doi.org/10.18710/sbr9gj/acb01p
https://dx.doi.org/10.18710/sbr9gj/qhx4ak
https://dx.doi.org/10.18710/sbr9gj/1z8m26
https://dx.doi.org/10.18710/sbr9gj/jwevh0
https://dx.doi.org/10.18710/sbr9gj/q95kqv
https://dx.doi.org/10.18710/sbr9gj/cixcbv
https://dx.doi.org/10.18710/sbr9gj/vog7lw
https://dx.doi.org/10.18710/sbr9gj/8pyecn
https://dx.doi.org/10.18710/sbr9gj/jntsbv
https://dx.doi.org/10.18710/sbr9gj/ba0pjg
https://dx.doi.org/10.18710/sbr9gj/7bzm3t
https://dx.doi.org/10.18710/sbr9gj/7giugg
https://dx.doi.org/10.18710/sbr9gj/flhoni
https://dx.doi.org/10.18710/sbr9gj/btr9eq
https://dx.doi.org/10.18710/sbr9gj/26lxk9
https://dx.doi.org/10.18710/sbr9gj/m0llrm
https://dx.doi.org/10.18710/sbr9gj/wfexpz
https://dx.doi.org/10.18710/sbr9gj/xqrnjd
https://dx.doi.org/10.18710/sbr9gj/vloe1i
https://dx.doi.org/10.18710/sbr9gj/gbxygm
op_doi https://doi.org/10.18710/sbr9gj10.18710/sbr9gj/acb01p10.18710/sbr9gj/qhx4ak10.18710/sbr9gj/1z8m2610.18710/sbr9gj/jwevh010.18710/sbr9gj/q95kqv10.18710/sbr9gj/cixcbv10.18710/sbr9gj/vog7lw10.18710/sbr9gj/8pyecn10.18710/sbr9gj/jntsbv10.18710/sbr9gj/ba0pjg10.1
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