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Crestal fault geometries reveal late halokinesis and collapse of the Samson Dome, Northern Norway: Implications for petroleum systems in the Barents Sea
This paper uses 2D and high-quality 3D seismic reflection data to assess the geometry and kinematics of the Samson Dome, offshore Norway, revising the implications of the new data to hydrocarbon exploration in the Barents Sea. The study area was divided into three (3) zones in terms of fault geometr...
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Published in: | Tectonophysics 2016-10, Vol.690, p.76-96 |
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description | This paper uses 2D and high-quality 3D seismic reflection data to assess the geometry and kinematics of the Samson Dome, offshore Norway, revising the implications of the new data to hydrocarbon exploration in the Barents Sea. The study area was divided into three (3) zones in terms of fault geometries and predominant strikes. Displacement-length (D-x) and Throw-depth (T-z) plots showed faults to consist of several segments that were later dip-linked. Interpreted faults were categorised into three families, with Type A comprising crestal faults, Type B representing large E-W faults, and Type C consisting of polygonal faults. The Samson Dome was formed in three major stages: a) a first stage recording buckling of the post-salt overburden and generation of radial faults; b) a second stage involving dissolution and collapse of the dome, causing subsidence of the overburden and linkage of initially isolated fault segments; and c) a final stage in which large fault segments were developed. Late Cretaceous faults strike predominantly to the NW, whereas NE-trending faults comprise Triassic structures that were reactivated in a later stage. Our work provides scarce evidence for the escape of hydrocarbons in the Samson Dome. In addition, fault analyses based on present-day stress distributions indicate a tendency for ‘locking’ of faults at depth, with the largest leakage factors occurring close to the surface. The Samson Dome is an analogue to salt structures in the Barents Sea where oil and gas exploration has occurred with varied degrees of success.
•3D seismic data are used to reassess the geometry and kinematics of the Samson Dome.•Faults crossing the dome were initiated in the Triassic and reactivated in several stages.•Faults show a tendency to ‘lock’ at depth under present-day stress conditions.•Samson Dome is a smaller seepage structure than previously proposed. |
doi_str_mv | 10.1016/j.tecto.2016.04.043 |
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•3D seismic data are used to reassess the geometry and kinematics of the Samson Dome.•Faults crossing the dome were initiated in the Triassic and reactivated in several stages.•Faults show a tendency to ‘lock’ at depth under present-day stress conditions.•Samson Dome is a smaller seepage structure than previously proposed.</description><identifier>ISSN: 0040-1951</identifier><identifier>EISSN: 1879-3266</identifier><identifier>DOI: 10.1016/j.tecto.2016.04.043</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Barents Sea ; Collapse ; Cretaceous ; Faults ; Fluid-flow ; Geometry ; Halokinesis ; Hydrocarbons ; Kinematics ; Natural gas ; Natural gas exploration ; Offshore ; Offshore drilling rigs ; Oil and gas exploration ; Oil exploration ; Petroleum ; Salt collapse ; Salts ; Samson Dome ; Segments ; Seismic surveys ; Structures ; Studies ; Tectonic stress ; Triassic</subject><ispartof>Tectonophysics, 2016-10, Vol.690, p.76-96</ispartof><rights>2016 The Authors</rights><rights>Copyright Elsevier BV Oct 28, 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a399t-17550c52cfcd898fa9f66183715652ff953b1089ad9f32ae9e05bfd0163114d73</citedby><cites>FETCH-LOGICAL-a399t-17550c52cfcd898fa9f66183715652ff953b1089ad9f32ae9e05bfd0163114d73</cites><orcidid>0000-0002-0668-3792</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Mattos, Nathalia H.</creatorcontrib><creatorcontrib>Alves, Tiago M.</creatorcontrib><creatorcontrib>Omosanya, Kamaldeen O.</creatorcontrib><title>Crestal fault geometries reveal late halokinesis and collapse of the Samson Dome, Northern Norway: Implications for petroleum systems in the Barents Sea</title><title>Tectonophysics</title><description>This paper uses 2D and high-quality 3D seismic reflection data to assess the geometry and kinematics of the Samson Dome, offshore Norway, revising the implications of the new data to hydrocarbon exploration in the Barents Sea. The study area was divided into three (3) zones in terms of fault geometries and predominant strikes. Displacement-length (D-x) and Throw-depth (T-z) plots showed faults to consist of several segments that were later dip-linked. Interpreted faults were categorised into three families, with Type A comprising crestal faults, Type B representing large E-W faults, and Type C consisting of polygonal faults. The Samson Dome was formed in three major stages: a) a first stage recording buckling of the post-salt overburden and generation of radial faults; b) a second stage involving dissolution and collapse of the dome, causing subsidence of the overburden and linkage of initially isolated fault segments; and c) a final stage in which large fault segments were developed. Late Cretaceous faults strike predominantly to the NW, whereas NE-trending faults comprise Triassic structures that were reactivated in a later stage. Our work provides scarce evidence for the escape of hydrocarbons in the Samson Dome. In addition, fault analyses based on present-day stress distributions indicate a tendency for ‘locking’ of faults at depth, with the largest leakage factors occurring close to the surface. The Samson Dome is an analogue to salt structures in the Barents Sea where oil and gas exploration has occurred with varied degrees of success.
•3D seismic data are used to reassess the geometry and kinematics of the Samson Dome.•Faults crossing the dome were initiated in the Triassic and reactivated in several stages.•Faults show a tendency to ‘lock’ at depth under present-day stress conditions.•Samson Dome is a smaller seepage structure than previously proposed.</description><subject>Barents Sea</subject><subject>Collapse</subject><subject>Cretaceous</subject><subject>Faults</subject><subject>Fluid-flow</subject><subject>Geometry</subject><subject>Halokinesis</subject><subject>Hydrocarbons</subject><subject>Kinematics</subject><subject>Natural gas</subject><subject>Natural gas exploration</subject><subject>Offshore</subject><subject>Offshore drilling rigs</subject><subject>Oil and gas exploration</subject><subject>Oil exploration</subject><subject>Petroleum</subject><subject>Salt collapse</subject><subject>Salts</subject><subject>Samson Dome</subject><subject>Segments</subject><subject>Seismic surveys</subject><subject>Structures</subject><subject>Studies</subject><subject>Tectonic stress</subject><subject>Triassic</subject><issn>0040-1951</issn><issn>1879-3266</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp9UU2PEzEMjRBIlIVfwMUSV6Ykk2Y6QeIA5WulFRwWzlE247ApmWRI0kX9J_xc3C1nJMtOrPds-T3Gngu-FlwMr_brhq7ldU-fNd9QyAdsJcat7mQ_DA_ZivMN74RW4jF7Uuuecz4INazYn13B2mwEbw-xwQ_MM7YSsELBO6R-tA3h1sb8MySsoYJNE7gco10qQvbQbhGu7VxzgvdEfglfcqFeSafHb3t8DZfzEoOzLeRUwecCC63IEQ8z1GNtOFcI6X7OO1swtQrXaJ-yR97Gis_-1Qv2_eOHb7vP3dXXT5e7t1edlVq3TmyV4k71zrtp1KO32g-DGOWWrlO991rJG8FHbSftZW9RI1c3fiKdpBCbaSsv2Ivz3KXkXwfSwuzzoSRaaUguKQfKilDyjHIl11rQm6WE2ZajEdycLDB7c2-BOVlg-IZCEuvNmYV0wF3AYqoLmBxOoRDYTDn8l_8XexSSyA</recordid><startdate>20161028</startdate><enddate>20161028</enddate><creator>Mattos, Nathalia H.</creator><creator>Alves, Tiago M.</creator><creator>Omosanya, Kamaldeen O.</creator><general>Elsevier B.V</general><general>Elsevier BV</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-0668-3792</orcidid></search><sort><creationdate>20161028</creationdate><title>Crestal fault geometries reveal late halokinesis and collapse of the Samson Dome, Northern Norway: Implications for petroleum systems in the Barents Sea</title><author>Mattos, Nathalia H. ; Alves, Tiago M. ; Omosanya, Kamaldeen O.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a399t-17550c52cfcd898fa9f66183715652ff953b1089ad9f32ae9e05bfd0163114d73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Barents Sea</topic><topic>Collapse</topic><topic>Cretaceous</topic><topic>Faults</topic><topic>Fluid-flow</topic><topic>Geometry</topic><topic>Halokinesis</topic><topic>Hydrocarbons</topic><topic>Kinematics</topic><topic>Natural gas</topic><topic>Natural gas exploration</topic><topic>Offshore</topic><topic>Offshore drilling rigs</topic><topic>Oil and gas exploration</topic><topic>Oil exploration</topic><topic>Petroleum</topic><topic>Salt collapse</topic><topic>Salts</topic><topic>Samson Dome</topic><topic>Segments</topic><topic>Seismic surveys</topic><topic>Structures</topic><topic>Studies</topic><topic>Tectonic stress</topic><topic>Triassic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mattos, Nathalia H.</creatorcontrib><creatorcontrib>Alves, Tiago M.</creatorcontrib><creatorcontrib>Omosanya, Kamaldeen O.</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Tectonophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mattos, Nathalia H.</au><au>Alves, Tiago M.</au><au>Omosanya, Kamaldeen O.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Crestal fault geometries reveal late halokinesis and collapse of the Samson Dome, Northern Norway: Implications for petroleum systems in the Barents Sea</atitle><jtitle>Tectonophysics</jtitle><date>2016-10-28</date><risdate>2016</risdate><volume>690</volume><spage>76</spage><epage>96</epage><pages>76-96</pages><issn>0040-1951</issn><eissn>1879-3266</eissn><abstract>This paper uses 2D and high-quality 3D seismic reflection data to assess the geometry and kinematics of the Samson Dome, offshore Norway, revising the implications of the new data to hydrocarbon exploration in the Barents Sea. The study area was divided into three (3) zones in terms of fault geometries and predominant strikes. Displacement-length (D-x) and Throw-depth (T-z) plots showed faults to consist of several segments that were later dip-linked. Interpreted faults were categorised into three families, with Type A comprising crestal faults, Type B representing large E-W faults, and Type C consisting of polygonal faults. The Samson Dome was formed in three major stages: a) a first stage recording buckling of the post-salt overburden and generation of radial faults; b) a second stage involving dissolution and collapse of the dome, causing subsidence of the overburden and linkage of initially isolated fault segments; and c) a final stage in which large fault segments were developed. Late Cretaceous faults strike predominantly to the NW, whereas NE-trending faults comprise Triassic structures that were reactivated in a later stage. Our work provides scarce evidence for the escape of hydrocarbons in the Samson Dome. In addition, fault analyses based on present-day stress distributions indicate a tendency for ‘locking’ of faults at depth, with the largest leakage factors occurring close to the surface. The Samson Dome is an analogue to salt structures in the Barents Sea where oil and gas exploration has occurred with varied degrees of success.
•3D seismic data are used to reassess the geometry and kinematics of the Samson Dome.•Faults crossing the dome were initiated in the Triassic and reactivated in several stages.•Faults show a tendency to ‘lock’ at depth under present-day stress conditions.•Samson Dome is a smaller seepage structure than previously proposed.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.tecto.2016.04.043</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0002-0668-3792</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Barents Sea Collapse Cretaceous Faults Fluid-flow Geometry Halokinesis Hydrocarbons Kinematics Natural gas Natural gas exploration Offshore Offshore drilling rigs Oil and gas exploration Oil exploration Petroleum Salt collapse Salts Samson Dome Segments Seismic surveys Structures Studies Tectonic stress Triassic |
title | Crestal fault geometries reveal late halokinesis and collapse of the Samson Dome, Northern Norway: Implications for petroleum systems in the Barents Sea |
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