Seismicity, focal mechanisms and morphology of subducted lithosphere in the Papua New Guinea-Solomon Islands region
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1985
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University of Hawaii at Manoa
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Abstract
The 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
Description
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Seismology, Geology, Structural, Seismology--Papua New Guinea., Seismology--Solomon Islands., Geology, Structural.
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Solomon Islands
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Theses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Geology and Geophysics
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