georefid:2007-128478SEDIS 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=10.1130/B26067.12007-01-01publicationgeorefid:2007-128478doi:10.1130/B26067.1Fletcher, John M.Centro de Investigacion Cientifica y de Educacion Superior de Ensenada, Departamento de Geologia, Ensenada, MexicoauthorGrove, MartyUniversity of California, Los Angeles, United StatesauthorKimbrough, DavidSan Diego State University, United StatesauthorLovera, OscarUniversity of Arizona, United StatesauthorGehrels, George E.authorGeological Society of America (GSA), Boulder, CO, United StatespublisherdocumentHardcopyGeological Society of America Bulletin119 (11-12)1313-1336The Magdalena fan is an apparently beheaded submarine depocenter that has figured prominently in reconstructions of middle to late Miocene Pacific-North American plate interactions. The deposit accumulated rapidly at the base of the continental slope on top of newly formed oceanic crust of the Magdalena microplate from 14.5 to 13 Ma. Subduction of this crust ceased as the Pacific-Magdalena spreading center encountered the trench. The widely accepted two-phase kinematic model for the formation of the Gulf of California holds that approximately 300 km of dextral shear between the Pacific and North American plates occurred along faults west of Baja California prior to the onset of dextral-transtensional shearing in the gulf ca. 6 Ma. We measured 1796 detrital zircon U-Pb ages from 65 samples in an effort to characterize the provenance of the fan, determine its source region, and define the cumulative dextral slip along faults offshore of southwestern Baja California. Zircons from the fan are dominantly 120-65 Ma with subordinate 15-35 Ma grains. Excellent matches to the fan can be obtained by mixing Magdalena shelf strata and/or adding detritus from the west-draining portion of the Los Cabos block. The same cannot be accomplished with zircons from the east-draining portion of the Los Cabos block and mainland Mexico. Our results favor a western Baja source region for the fan and suggest that cumulative dextral slip along faults west of Baja was <150 km, much less than previously believed. We propose that the fan was fed by erosional denudation of the Magdalena shelf produced by increased mantle buoyancy due to the ridge-trench juxtaposition. The fan's source was cut off when faults west of Baja California began to accommodate transtensional shearing and form rift basins that captured detritus that previously reached the trench.completedSolid-earth geophysicsGeochronologyabsolute ageBaja California Sur MexicoCenozoicclastic rocksclastic sedimentsComondu Formationcontinental shelfdatesDeep Sea Drilling ProjectdenudationdetritusDSDP Site 421East PacificerosionfaultsGulf of CaliforniaIntegrated Ocean Drilling ProgramIPODkinematicsLeg 54Magdalena Fanmarine sedimentsMexicoMioceneNeogenenesosilicatesNorth American PlateNorth PacificNortheast Pacificocean floorsorthosilicatesPacific OceanPacific PlatePESCADEROplate tectonicsprogramsprovenanceSan Gregorio Formationsandsandstonesea-floor spreadingsedimentary rockssedimentsshearsilicatesspreading centerssubmarine fansTepetate FormationTertiarytranstensiontrenchesU/Pbupper Miocenezirconzircon groupurn:org.iodp:exp:54urnlargerWorkCitationcampaignurn:org.iodp:exp:54:site:421urnlargerWorkCitationstudyurn:org.iodp:exp:54urnlargerWorkCitationcampaignEnglishgeoscientificInformation-114.0000-104.000020.000026.3000With GSA Data Repository Item 2007194