Paleocene arc-continent collision in southeastern Papua New Guinea was followed in the Neogene by 50 km of extension on low-angle faults, emplacement of intrusive rocks, uplift and tilting and erosion to reveal the PUB ophiolite

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ADS bibcode
2012AGUFM.T42C..05D
year
2012
Listed Authors
Davies, H. L.
Jonda, L.
Listed Institutions
Earth Sciences, University of PNG, UNIVERSITY NCD, Papua New Guinea;
Earth Sciences, University of PNG, UNIVERSITY NCD, Papua New Guinea;

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