<?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:1985-006080</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=1985-006080</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Etude de la transition continent-ocean sur la marge continentale Nord Gascone a partir des documents enregistres lors de la campagne sismique refraction a deux bateaux IPOD 79 Study of land to ocean transition on the continental margin of northern Bay of Biscay from data recorded in the frame of IPOD 79 two-ship refraction seismics campaign</gco:CharacterString></title><date><CI_Date><date><gco:Date>1981-01-01</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:1985-006080</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Camus, Anne-Lise</gco:CharacterString></individualName><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><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><page><gco:CharacterString>373 pp.</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>This memoir, prepared in the frame the IPOD 79 expedition, aims at specifying, through refraction seismics, the transition between oceanic and continental crusts in N Bay of Biscay. The data were recorded in July 1979 during an original campaign involving two ships. The seismic lines were laid in the various zones: continental, transition, oceanic zones. In order to attain the selected objectives (determination of discontinuities down to mantle), several seismic methods were applied on the various lines: conventional reflection, central common point line, fixed distance (30 km and 5 km) line, receivers laid on sea floor (OBS). These data were processed by means of newly developed programs. A model of geological structures (velocity, depth and trend of discontinuities) across the continental margin of N Bay of Biscay could finally be worked out</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>Solid-earth geophysics</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Bay of Biscay</gco:CharacterString></keyword><keyword><gco:CharacterString>block structures</gco:CharacterString></keyword><keyword><gco:CharacterString>common-depth-point method</gco:CharacterString></keyword><keyword><gco:CharacterString>continental crust</gco:CharacterString></keyword><keyword><gco:CharacterString>crust</gco:CharacterString></keyword><keyword><gco:CharacterString>data processing</gco:CharacterString></keyword><keyword><gco:CharacterString>faults</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical methods</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical surveys</gco:CharacterString></keyword><keyword><gco:CharacterString>marine methods</gco:CharacterString></keyword><keyword><gco:CharacterString>Mohorovicic discontinuity</gco:CharacterString></keyword><keyword><gco:CharacterString>North Atlantic</gco:CharacterString></keyword><keyword><gco:CharacterString>oceanic crust</gco:CharacterString></keyword><keyword><gco:CharacterString>passive margins</gco:CharacterString></keyword><keyword><gco:CharacterString>plate tectonics</gco:CharacterString></keyword><keyword><gco:CharacterString>reflection methods</gco:CharacterString></keyword><keyword><gco:CharacterString>refraction methods</gco:CharacterString></keyword><keyword><gco:CharacterString>seismic methods</gco:CharacterString></keyword><keyword><gco:CharacterString>structural geology</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>theses</gco:CharacterString></keyword></MD_Keywords></descriptiveKeywords><language><gco:CharacterString>French</gco:CharacterString></language><topicCategory><MD_TopicCategoryCode>geoscientificInformation</MD_TopicCategoryCode></topicCategory><extent><EX_Extent><geographicElement><EX_GeographicBoundingBox><westBoundLongitude><gco:Decimal>-8.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>-1.1000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>43.2000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>48.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>Bay of Biscay</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>