<?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:1968-061355</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=1968-061355</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Geophysical oceanographic studies at Lamont Geological Observatory</gco:CharacterString></title><date><CI_Date><date><gco:Date>1968-01-01</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:1968-061355</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Ewing, Maurice</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><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Worzel, J. Lamar</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><name><gco:CharacterString>In: Selected papers from the Governor's Conference on Oceanography, New York, 1967</gco:CharacterString></name><page><gco:CharacterString>8-35</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>Development of underwater cameras, depth sounding instruments, piston corers, seismic refraction, gravity, and magnetic measurements is described. Improvement of heat-flow measurements, and development of a large volume water sampler are among outstanding advances cited. The trend is to include more and more instruments in a single package. A very extensive Upper Cretaceous subbottom reflector has been identified in the Atlantic and the upper structure of the continental shelves of North America has been delineated. Structure sections of the Blake Plateau resulting from the first JOIDES project are shown. An example of the results of a combined study is shown on a map of the north Pacific.</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>Structural geology</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Blake Plateau</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>continental shelf</gco:CharacterString></keyword><keyword><gco:CharacterString>Cretaceous</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical methods</gco:CharacterString></keyword><keyword><gco:CharacterString>Holocene</gco:CharacterString></keyword><keyword><gco:CharacterString>instruments</gco:CharacterString></keyword><keyword><gco:CharacterString>JOIDES</gco:CharacterString></keyword><keyword><gco:CharacterString>measurement</gco:CharacterString></keyword><keyword><gco:CharacterString>Mesozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>North America</gco:CharacterString></keyword><keyword><gco:CharacterString>North Atlantic</gco:CharacterString></keyword><keyword><gco:CharacterString>North Pacific</gco:CharacterString></keyword><keyword><gco:CharacterString>oceanography</gco:CharacterString></keyword><keyword><gco:CharacterString>Pacific Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Quaternary</gco:CharacterString></keyword><keyword><gco:CharacterString>reflection methods</gco:CharacterString></keyword><keyword><gco:CharacterString>structural geology</gco:CharacterString></keyword><keyword><gco:CharacterString>techniques</gco:CharacterString></keyword><keyword><gco:CharacterString>Upper Cretaceous</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>-173.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>20.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>0.0000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>84.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>North America</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>North Atlantic</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>