<?xml version="1.0" encoding="UTF-8" ?><MD_Metadata xmlns="http://www.isotc211.org/2005/gmd" xmlns:gco="http://www.isotc211.org/2005/gco" xmlns:gml="http://www.opengis.net/gml" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.isotc211.org/2005/gmd http://www.isotc211.org/2005/gmd/gmd.xsd"><fileIdentifier><gco:CharacterString>georefid:1984-056284</gco:CharacterString></fileIdentifier><contact><CI_ResponsibleParty><organisationName><gco:CharacterString>SEDIS Publication Catalogue</gco:CharacterString></organisationName><contactInfo><CI_Contact><address><CI_Address><electronicMailAddress><gco:CharacterString>ana.macario@awi.de</gco:CharacterString></electronicMailAddress></CI_Address></address><onlineResource><CI_OnlineResource><linkage><URL>http://sedis.iodp.org/pub-catalogue/</URL></linkage><function><CI_OnLineFunctionCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode_information">information</CI_OnLineFunctionCode></function></CI_OnlineResource></onlineResource></CI_Contact></contactInfo><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_pointOfContact">pointOfContact</CI_RoleCode></role></CI_ResponsibleParty></contact><dateStamp><gco:DateTime>2011-06-23T00:00:00Z</gco:DateTime></dateStamp><dataSetURI><gco:CharacterString>http://sedis.iodp.org/pub-catalogue/index.php?id=1984-056284</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Cenozoic and late Mesozoic stratigraphy and subsidence history of the Norwegian margin</gco:CharacterString></title><date><CI_Date><date><gco:Date>1984-01-01</gco:Date></date><dateType><CI_DateTypeCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode_publication">publication</CI_DateTypeCode></dateType></CI_Date></date><identifier><MD_Identifier><code><gco:CharacterString>georefid:1984-056284</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Mutter, John C.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Lamont-Doherty Geol. Obs., Palisades, NY, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><organisationName><gco:CharacterString>Geological Society of America (GSA), Boulder, CO, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_publisher">publisher</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><presentationForm><CI_PresentationFormCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode_documentHardcopy">documentHardcopy</CI_PresentationFormCode></presentationForm><series><CI_Series><name><gco:CharacterString>Geological Society of America Bulletin</gco:CharacterString></name><issueIdentification><gco:CharacterString>95 (10)</gco:CharacterString></issueIdentification><page><gco:CharacterString>1135-1149</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>DSDP data at five sites on the outer margin and multichannel seismic data. The margin can be divided into three physiographic provinces: two broad shelf and slope regions separated by the Jan Mayen fracture zone, and the steep, narrow shelf and slope off the Lofoten Islands. Each experienced a separate Cenozoic subsidence history. The Voering Plateau is partly underlain by oceanic crust; it subsided nearly 1,000 m less than expected from thermal contraction, but it did so following the development of a relatively deep-water environment in the Paleocene. North of the Voering Plateau, the margin may have subsided a few hundred meters more than thermal studies had predicted. There is no evidence for a phase of extensional deformation associated with the inception of spreading. The youngest faulted level occurs at the Late Jurassic level, preceding sea-floor spreading by nearly 100 Ma, and deformation in the Cretaceous section is characterized by large uplift structures that may be of halokinetic origin.--Modified journal abstract.</gco:CharacterString></abstract><status><MD_ProgressCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode_completed">completed</MD_ProgressCode></status><descriptiveKeywords><MD_Keywords><keyword><gco:CharacterString>Oceanography</gco:CharacterString></keyword><keyword><gco:CharacterString>Arctic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>bathymetry</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>continental margin</gco:CharacterString></keyword><keyword><gco:CharacterString>continental shelf</gco:CharacterString></keyword><keyword><gco:CharacterString>continental slope</gco:CharacterString></keyword><keyword><gco:CharacterString>controls</gco:CharacterString></keyword><keyword><gco:CharacterString>cores</gco:CharacterString></keyword><keyword><gco:CharacterString>Cretaceous</gco:CharacterString></keyword><keyword><gco:CharacterString>crust</gco:CharacterString></keyword><keyword><gco:CharacterString>Europe</gco:CharacterString></keyword><keyword><gco:CharacterString>extension tectonics</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical methods</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical profiles</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical surveys</gco:CharacterString></keyword><keyword><gco:CharacterString>Jan Mayen Ridge</gco:CharacterString></keyword><keyword><gco:CharacterString>Jurassic</gco:CharacterString></keyword><keyword><gco:CharacterString>marine sedimentation</gco:CharacterString></keyword><keyword><gco:CharacterString>marine sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>Mesozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>multichannel filters</gco:CharacterString></keyword><keyword><gco:CharacterString>Norway</gco:CharacterString></keyword><keyword><gco:CharacterString>Norwegian Sea</gco:CharacterString></keyword><keyword><gco:CharacterString>oceanic crust</gco:CharacterString></keyword><keyword><gco:CharacterString>oceanography</gco:CharacterString></keyword><keyword><gco:CharacterString>passive margins</gco:CharacterString></keyword><keyword><gco:CharacterString>physiographic provinces</gco:CharacterString></keyword><keyword><gco:CharacterString>salt tectonics</gco:CharacterString></keyword><keyword><gco:CharacterString>Scandinavia</gco:CharacterString></keyword><keyword><gco:CharacterString>sea-floor spreading</gco:CharacterString></keyword><keyword><gco:CharacterString>sedimentation</gco:CharacterString></keyword><keyword><gco:CharacterString>sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>seismic methods</gco:CharacterString></keyword><keyword><gco:CharacterString>stratigraphy</gco:CharacterString></keyword><keyword><gco:CharacterString>structural controls</gco:CharacterString></keyword><keyword><gco:CharacterString>subsidence</gco:CharacterString></keyword><keyword><gco:CharacterString>surveys</gco:CharacterString></keyword><keyword><gco:CharacterString>tectonics</gco:CharacterString></keyword><keyword><gco:CharacterString>tectonophysics</gco:CharacterString></keyword><keyword><gco:CharacterString>Upper Jurassic</gco:CharacterString></keyword><keyword><gco:CharacterString>Voring Plateau</gco:CharacterString></keyword><keyword><gco:CharacterString>Western Europe</gco:CharacterString></keyword></MD_Keywords></descriptiveKeywords><language><gco:CharacterString>English</gco:CharacterString></language><topicCategory><MD_TopicCategoryCode>geoscientificInformation</MD_TopicCategoryCode></topicCategory><extent><EX_Extent><geographicElement><EX_GeographicBoundingBox><westBoundLongitude><gco:Decimal>0.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>14.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>63.0000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>69.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>