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Convergent tectonics in the Huon Peninsula region,Papua New Guinea
Authors:H. L. Davies  J. Lock  D. L. Tiffin  E. Honza  Y. Okuda  F. Murakami  K. Kisimoto
Affiliation:(1) Bureau of Mineral Resources, GPO Box 378, 2601 Canberra, Australia;(2) Present address: CCOP/SOPAC, Private Mail Bag, Suva, Fiji;(3) Geological Survey of Japan, Tsukuba, Japan
Abstract:The anticlinal nappe which forms the Huon Peninsula and adjacent ranges extends offshore as the Huon Ridge. The frontal thrust of the nappe is the Ramu-Markham Fault (onshore) and a deformation front along the line of the Markham Canyon (offshore). The timing and geometry of the Finisterre arc-continent collision is controversial, and the origin of the Finsch Deep is unresolved.
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