georefid:2010-063341SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-07-06T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2010-063341<gco:CharacterString>A change in slip mechanism and subsequent weakening along a fault zone in in-situ magmatic oceanic crust, 30 degrees N Mid-Atlantic Ridge</gco:CharacterString>2005-01-01publicationgeorefid:2010-063341Michibayashi, K.Shizuoka University, Institute of Geosciences, Shizuoka, JapanauthorEscartin, J.Institut de Physique du Globe de Paris, FranceauthorDelius, H.University of Leicester, United KingdomauthorLinek, M.RWTH Aachen University, Federal Republic of GermanyauthorNozaka, T.Okayama University, JapanauthorHirose, T.Kyoto University, JapanauthorOhara, Y.Hydrographic and Oceanographic Department of Japan, JapanauthorAmerican Geophysical Union, Washington, DC, United StatespublisherdocumentHardcopyIn: Anonymous, AGU 2005 fall meeting86 (52, Suppl.)completedSolid-earth geophysicsStructural geologyAtlantic OceanAtlantis Massifboreholeschloritechlorite groupcrustdeformationExpeditions 304/305fault zonesfaultsgabbrosigneous rocksimage analysisIntegrated Ocean Drilling ProgrammagmatismMid-Atlantic RidgeNorth Atlanticoceanic crustolivine gabbroplutonic rocksshear zonessheet silicatessilicatessubduction zonestectonicsEnglishgeoscientificInformation-80.000020.0000-57.000075.0000Expeditions 304/305Mid-Atlantic RidgeNorth Atlantic