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dc.contributor.authorPurdy, G. Michael  Concept link
dc.contributor.authorDetrick, Robert S.  Concept link
dc.date.accessioned2018-05-30T17:55:30Z
dc.date.available2018-05-30T17:55:30Z
dc.date.issued1979-02
dc.identifier.urihttps://hdl.handle.net/1912/10396
dc.descriptionAlso published as: Journal of Geophysical Research 83 (1978): 2247-2257en_US
dc.description.abstractA seismic refraction experiment in the central Banda Sea is interpreted by using both slope intercept and delay time function methods. The crustal structure is shown to be oceanic, with velocities (4.97, 6.47, 7.18, and 7.97 km/s) typical of oceanic layers 2, 3A, and 3B and the mantle. Individual layer thicknesses va ry systematica lly along the line, though the range of thicknesses observed for layers 2 ( 1.5-2.0 km) and 3A (2.0-3.5 km) falls well within the range observed for normal oceanic crust. Layer 3B is unusually thick (2.5-4.6 km), the result being slightl y greater than normal depths-to Moho of9-IO km below the sea floor. Shear head waves from layers 3A and 3B are identified on two receivers. In both cases, shear wave conversion occurred at the sediment/layer 2 interface. The observed shear wave velocities and intercepts indicate a Poisson's ratio of 0.25-0.28 in layer 3 and ~0.33 in layer 2. These and earlier results from the southern Banda basin indicate that the entire Banda Sea is underlain by oceanic type crust.en_US
dc.description.sponsorshipPrepared for the Office of Naval Research under Contract N00014-74-C-0262; NR 083-004 and for the International Decade of Ocean Exploration of the National Science Foundation under Grant OCE 75-19150.en_US
dc.language.isoen_USen_US
dc.publisherWoods Hole Oceanographic Institutionen_US
dc.relation.ispartofseriesWHOI Technical Reportsen_US
dc.relation.ispartofseriesWHOI-79-20en_US
dc.subjectSeismic refraction methoden_US
dc.titleA seismic refraction experiment in the central Banda Seaen_US
dc.typeTechnical Reporten_US
dc.identifier.doi10.1575/1912/10396


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