Lin, Thomas Tung-Hung and Ledbetter, Michael T. (1984): Distribution of volcanic ash reflectors in the eastern equatorial Pacific Ocean

Leg/Site/Hole:
Identifier:
1984-050819
georefid

Creator:
Lin, Thomas Tung-Hung
Univ. Ga., Dep. Geol., Athens, GA, United States
author

Ledbetter, Michael T.
author

Identification:
Distribution of volcanic ash reflectors in the eastern equatorial Pacific Ocean
1984
Marine Geology
Elsevier, Amsterdam, Netherlands
59
1-4
251-269
Twelve 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.
English
Serial
Coverage:Geographic coordinates:
North:12.0000
West:-95.0000East: -80.0000
South:2.0000

Oceanography; acoustical methods; Cenozoic; Central America; cores; East Pacific; Equatorial Pacific; eruptions; geophysical methods; geophysical surveys; marine sediments; Mexico; North American Pacific; North Pacific; Northeast Pacific; Pacific Ocean; provenance; Quaternary; sedimentation; sediments; seismic methods; South America; surveys; volcaniclastics; volcanism; volcanology; wind transport;

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