georefid:1997-049749SEDIS Publication Catalogue
ana.macario@awi.de
http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=1997-049749<gco:CharacterString>The relationship between hydrothermal flow and sedimentary diagenesis, structure, and texture in distal turbidites of Middle Valley of the Juan de Fuca Ridge, ODP Leg 139</gco:CharacterString>1996-01-01publicationgeorefid:1997-049749Higgins, K. M.East Carolina University, Departmnet of Geology, Greenville, NC, United StatesauthorRigsby, C. A.Duke University, United StatesauthorBaker, P. A.Universitat Bern, SwitzerlandauthorBurns, S. J.authorGeological Society of America (GSA), Boulder, CO, United StatespublisherdocumentHardcopyIn: Anonymous, Geological Society of America, 28th annual meeting28 (7)214completedSedimentary petrologyalkaline earth metalsalterationburrowsC-13/C-12carboncarbon dioxidecoresdepositional environmentdiagenesisEast Pacificgeothermal gradientheat flowhemipelagic environmenthydrothermal conditionshydrothermal ventsironisotope ratiosisotopesJuan de Fuca RidgeLeg 139magnesiummanganesemarine environmentmetalsMiddle Valleymineral compositionNorth PacificNortheast PacificO-18/O-16Ocean Drilling ProgramoxidationoxygenPacific Oceanpaleotemperaturepelagic environmentreductionsea-floor spreadingsedimentationsedimentation ratesstable isotopesstrontiumtexturesturbiditeX-ray datazincurn:org.iodp:exp:139urnlargerWorkCitationcampaignEnglishgeoscientificInformation-128.4250-128.381548.260048.2730