<?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:2005-046429</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=10.1111/j.1365-2117.2004.00242.x</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Late Cretaceous and Cenozoic sea-level estimates; backstripping analysis of borehole data, onshore New Jersey</gco:CharacterString></title><date><CI_Date><date><gco:Date>2004-01-01</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:2005-046429</gco:CharacterString></code></MD_Identifier></identifier><identifier><MD_Identifier><code><gco:CharacterString>doi:10.1111/j.1365-2117.2004.00242.x</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Van Sickel, William A.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Western Michigan University, Department of Geosciences, Kalamazoo, MI, 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><individualName><gco:CharacterString>Kominz, Michelle A.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Rutgers University, 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><individualName><gco:CharacterString>Miller, Kenneth G.</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>Browning, James V.</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><organisationName><gco:CharacterString>Blackwell Science, Oxford, United Kingdom</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>Basin Research</gco:CharacterString></name><issueIdentification><gco:CharacterString>16 (4)</gco:CharacterString></issueIdentification><page><gco:CharacterString>451-465</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>Backstripping analysis of the Bass River and Ancora boreholes from the New Jersey coastal plain (Ocean Drilling Project Leg 174AX) provides new Late Cretaceous sea-level estimates and corroborates previously published Cenozoic sea-level estimates. Compaction histories of all coastal plain boreholes were updated using porosity-depth relationships estimated from New Jersey coastal plain electric logs. The new porosity estimates are considerably lower than those previously calculated at the offshore Cost B-2 well. Amplitudes and durations of sea-level variations are comparable in sequences that are represented at multiple boreholes, suggesting that the resultant curves are an approximation of regional sea level. Both the amplitudes and durations of third-order (0.5-5 Myr) cycles tend to decrease from the Late Cretaceous to the late Miocene. Third-order sea-level amplitudes in excess of 60 m are not observed. Long-term (10 (super 8) -10 (super 7) years) sea level was approximately constant at 30-80 m in the Late Cretaceous, rose to a maximum early Eocene value of approximately 100-140 m, and then fell through the Eocene and Oligocene.</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>Stratigraphy</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic Coastal Plain</gco:CharacterString></keyword><keyword><gco:CharacterString>boreholes</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>Central Atlantic Coastal Plain</gco:CharacterString></keyword><keyword><gco:CharacterString>coastal plains</gco:CharacterString></keyword><keyword><gco:CharacterString>Cretaceous</gco:CharacterString></keyword><keyword><gco:CharacterString>data bases</gco:CharacterString></keyword><keyword><gco:CharacterString>data processing</gco:CharacterString></keyword><keyword><gco:CharacterString>depth</gco:CharacterString></keyword><keyword><gco:CharacterString>Eocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Leg 174AX</gco:CharacterString></keyword><keyword><gco:CharacterString>Mesozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>Miocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Neogene</gco:CharacterString></keyword><keyword><gco:CharacterString>New Jersey</gco:CharacterString></keyword><keyword><gco:CharacterString>Ocean Drilling Program</gco:CharacterString></keyword><keyword><gco:CharacterString>Oligocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Paleogene</gco:CharacterString></keyword><keyword><gco:CharacterString>porosity</gco:CharacterString></keyword><keyword><gco:CharacterString>sea-level changes</gco:CharacterString></keyword><keyword><gco:CharacterString>sedimentation</gco:CharacterString></keyword><keyword><gco:CharacterString>sedimentation rates</gco:CharacterString></keyword><keyword><gco:CharacterString>Tertiary</gco:CharacterString></keyword><keyword><gco:CharacterString>United States</gco:CharacterString></keyword><keyword><gco:CharacterString>Upper Cretaceous</gco:CharacterString></keyword><keyword><gco:CharacterString>upper Miocene</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>-76.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>-72.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>38.5000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>41.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>