<?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:1983-031614</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=1983-031614</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Geotechnical properties of two calcareous oozes</gco:CharacterString></title><date><CI_Date><date><gco:Date>1982-01-01</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:1983-031614</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Valent, P. J.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Brian Watt Assoc., Houston, TX, 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>Altschaeffl, A. G.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Humboldt State Univ., Arcata, CA, 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>Lee, H. J.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Purdue Univ., West Lafayette, IN, 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>American Society for Testing and Materials, Philadelphia, PA, 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>In: Demars, K. R. (editor), Chaney, R. C. (editor), Geotechnical properties, behavior, and performance of calcareous soils</gco:CharacterString></name><issueIdentification><gco:CharacterString>777</gco:CharacterString></issueIdentification><page><gco:CharacterString>79-96</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>The first ooze, a clayey silt with 56 to 75 percent calcium carbonate, was subjected to laboratory vane shear, one-dimensional compression, and triaxial shear testing. The void ratio-log pressure relationship obtained from one-dimensional compression tests, for a pressure increment ratio of 1, was found to be continuously plunging, a curve form possibly characteristic of the calcareous oozes. The failure envelope determined from triaxial shear tests defined a decreasing effective friction angle with increasing confining stress (34 deg. decreasing to 28 deg.). Effort toward establishing a connection between these phenomena and grain crushing in the sediment at engineering loads were not conclusive. The second ooze, a fine sand-silt with 77 to 86 percent calcium carbonate, was tested both in-place (vane shear) and in the laboratory (vane shear and triaxial). In-place vane strengths are quite high, 10 to 30 kPa (1.5 to 4.5 psi), while laboratory vane strengths are near zero. The ooze exhibits high in-place vane strength sensitivities (5 to 10).--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>Engineering geology</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Beata Ridge</gco:CharacterString></keyword><keyword><gco:CharacterString>calcareous composition</gco:CharacterString></keyword><keyword><gco:CharacterString>Calcareous soils</gco:CharacterString></keyword><keyword><gco:CharacterString>Caribbean Sea</gco:CharacterString></keyword><keyword><gco:CharacterString>clastic sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>compression</gco:CharacterString></keyword><keyword><gco:CharacterString>Deep Sea Drilling Project</gco:CharacterString></keyword><keyword><gco:CharacterString>DSDP Site 146/149</gco:CharacterString></keyword><keyword><gco:CharacterString>engineering geology</gco:CharacterString></keyword><keyword><gco:CharacterString>materials, properties</gco:CharacterString></keyword><keyword><gco:CharacterString>North Atlantic</gco:CharacterString></keyword><keyword><gco:CharacterString>one-dimensional models</gco:CharacterString></keyword><keyword><gco:CharacterString>ooze</gco:CharacterString></keyword><keyword><gco:CharacterString>sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>shear</gco:CharacterString></keyword><keyword><gco:CharacterString>soil mechanics</gco:CharacterString></keyword><keyword><gco:CharacterString>soils</gco:CharacterString></keyword><keyword><gco:CharacterString>triaxial tests</gco:CharacterString></keyword><keyword><gco:CharacterString>Venezuelan Basin</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>-69.2000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>-69.2000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>15.0000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>15.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>