Seismicity, focal mechanisms and morphology of subducted lithosphere in the Papua New Guinea-Solomon Islands region

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dc.contributor.authorCooper, Patricia Ann
dc.contributor.departmentGeology and Geophysics
dc.date.accessioned2021-09-13T19:30:15Z
dc.date.available2021-09-13T19:30:15Z
dc.date.issued1985
dc.description.abstractThe Papua New Guinea-Solomon Islands region is a major component of the Western Melanesian Borderlands, the convergent boundary between the northward-moving Inda-Australian Plate and the westwardmoving Pacific Plate (Figure 1.1). The region represents a w
dc.description.degreePh.D.
dc.identifier.urihttp://hdl.handle.net/10125/76138
dc.languageeng
dc.publisherUniversity of Hawaii at Manoa
dc.relationTheses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Geology and Geophysics
dc.subjectSeismology
dc.subjectGeology, Structural
dc.subject.lcshSeismology--Papua New Guinea.
dc.subject.lcshSeismology--Solomon Islands.
dc.subject.lcshGeology, Structural.
dc.titleSeismicity, focal mechanisms and morphology of subducted lithosphere in the Papua New Guinea-Solomon Islands region
dc.typeThesis
dc.type.dcmiText
dcterms.spatialSolomon Islands
local.identifier.callnumberAC1 .H3 no.1947
local.identifier.voyagerid535688

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