georefid:1984-050819SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=1984-050819<gco:CharacterString>Distribution of volcanic ash reflectors in the eastern equatorial Pacific Ocean</gco:CharacterString>1984-01-01publicationgeorefid:1984-050819Lin, Thomas Tung-HungUniv. Ga., Dep. Geol., Athens, GA, United StatesauthorLedbetter, Michael T.authorElsevier, Amsterdam, NetherlandspublisherdocumentHardcopyMarine Geology59 (1-4)251-269Twelve discrete reflectors within 40 m of the seafloor may be traced in the region. Shallow (<20 m) seismic reflectors can be correlated to ash layers in piston cores. In addition, deeper seismic reflectors (>20 m) can be correlated with ash layers in two DSDP cores and used to indirectly establish that all seismic reflectors in this study are ash layers. Based on areal distribution patterns, most seismic reflectors indicate the direction of possible volcanic sources. Moreover, using an assumed constant sedimentation rate of 3 CM X 10 (super 3) yr-1) , the average estimated age of each reflector can be calculated. All ash reflectors are Quaternary in age. Reflectors 1 to 3 are correlated to marine ash layers "D", "I", and "L", and the assigned ages correlate well with the previously established ages of 83,000, 133,000 and 230,000 yrs B.P., respectively, for these layers.--Modified journal abstract.completedOceanographyacoustical methodsCenozoicCentral AmericacoresEast PacificEquatorial Pacificeruptionsgeophysical methodsgeophysical surveysmarine sedimentsMexicoNorth American PacificNorth PacificNortheast PacificPacific OceanprovenanceQuaternarysedimentationsedimentsseismic methodsSouth Americasurveysvolcaniclasticsvolcanismvolcanologywind transportEnglishgeoscientificInformation-95.0000-80.00002.000012.0000