georefid:1983-042924SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1029/JB088iB03p02337<gco:CharacterString>Velocity and attenuation anisotropy in deep-sea carbonate sediments</gco:CharacterString>1983-01-01publicationgeorefid:1983-042924doi:10.1029/JB088iB03p02337Kim, Dae-ChoulHawaii Inst. Geophys., Honolulu, HI, United StatesauthorKatahara, Keith W.authorManghnani, Murli H.authorSchlanger, Seymour O.authorAmerican Geophysical Union, Washington, DC, United StatespublisherdocumentDigitalJournal of Geophysical Research88 (B3)2337-2343Laboratory studies, Deep Sea Drilling Project Site 288 on the Ontong Java Plateau. Velocity anisotropy for compressional waves is found to decrease with increasing effective pressure, i.e., with closure of pores. Preferred horizontal orientation is also a significant cause of the observed anisotropy.--Modified journal abstract.completedGeneral geophysicsacoustical propertiesanisotropyattenuationbody wavescarbonate sedimentsDeep Sea Drilling Projectdeep-sea environmentdiagenesisDSDP Site 288effectselastic wavesexperimental studiesLeg 30marine environmentmarine sedimentsmaterials, propertiesOntong Java PlateauP-wavesPacific Oceanphysical propertiespore pressureporositypreferred orientationpressurepropertiesS-wavessedimentsseismic wavesseismologysoil mechanicsvelocityWest Pacificurn:org.iodp:exp:30urnlargerWorkCitationcampaignurn:org.iodp:exp:30:site:288urnlargerWorkCitationstudyurn:org.iodp:exp:30urnlargerWorkCitationcampaignEnglishgeoscientificInformation153.0000176.0000-27.00000.0000Hawaii Inst. Geophys.; Contrib. No. 1334application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www.agu.org/journals/jb/v088/iB03/JB088iB03p02337/JB088iB03p02337.pdfdownload