georefid:1982-051676SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=1982-051676<gco:CharacterString>Tectonique, volcanisme, morphologies et climats cenozoiques au large du Japon, d'apres la sedimentation argileuse marine Tectonics, volcanism, morphology and Cenozoic climate off Japan, as determined from marine clay sedimentation</gco:CharacterString>1981-01-01publicationgeorefid:1982-051676Chamley, H.Univ. Lille I, sedimentol. geochim., Villeneuve d'Ascq 59655, United StatesauthorCadet, J. P.authorGauthier-Villars, Montrouge, FrancepublisherdocumentHardcopyComptes Rendus des Seances de l'Academie des Sciences, Serie 2: Mecanique, Physique, Chimie, Sciences de la Terre, Sciences de l'Univers292 (2)219-224The argillaceous sequence identified on the inner margin of the Japan Trench (DSDP Leg 57) is in accordance with the existence of the ancient continent "Oyashio". Probably present in the Cretaceous, the continent subsided during latest Oligocene time. At the beginning of the Miocene, the reconstruction of the ocean floor led to the expansion of the role of provenance, and of that of the Japanese climate, in controlling sedimentation.completedSedimentary petrologyareal studiesAsiaCenozoicclastic sedimentsclayclay mineralogyclay mineralsCretaceousDeep Sea Drilling Projectdeep-sea environmentdeep-sea sedimentationenvironmentFar EastIPODJapanJapan TrenchLeg 57marine environmentmarine sedimentationmarine sedimentsMesozoicmineral assemblagesNeogeneNorth PacificNorthwest PacificOligocenePacific OceanpaleoclimatologyPaleogenepaleogeographyPleistoceneQuaternaryreconstructionsedimentationsedimentssheet silicatessilicatesstratigraphic gapsstratigraphyTertiaryUpper Cretaceousupper OligoceneWest Pacificurn:org.iodp:exp:57urnlargerWorkCitationcampaignFrenchgeoscientificInformation143.1500143.150040.400040.4000