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  1. 1 de mar. de 2012 · Davies, H. L. , 2012, The geology of New Guinea - the cordilleran margin of the Australian continent. Episodes 35(1), 87-102.

  2. www.academia.edu › 101259071 › The_geology_of_New_Guinea_the_cordilleran_margin_ofThe geology of New Guinea - Academia.edu

    87 by Hugh L. Davies The geology of New Guinea - the cordilleran margin of the Australian continent Earth Sciences, University of Papua New Guinea, PO Box 414, University NCD, ... The basement is exposed in the mountains S of Episodes Vol. 35, no. 1 88 the present day” (Pieters et al., 1983) ...

  3. H. DAVIES, Chamber of Mines Professor of Applied Geology | Cited by 3,349 | of University of Papua New Guinea, Port Moresby (UPNG) | Read 169 publications | Contact H. DAVIES

  4. 20 de jul. de 2021 · Davies, H.L. The geology of New Guinea—the cordilleran margin of the Australian continent. Episodes 2012, 35, 87–102. [Google Scholar] Howe, B.; Kroll, A. The Geophysical Response of the Tupinda Cu-Au-Mo Porphyry Prospect, Tabar Islands, Papua New Guinea. ASEG Ext. Abstr. 2010, 2010, 1–5.

  5. 4 de ago. de 2015 · Davies HL (2012) The geology of New Guinea—the cordilleran margin of the Australian continent. Episodes 35(1):87102. Google Scholar Davies HL, Jaques AL (1984) Emplacement of ophiolite in Papua New Guinea. Special publication. Geological Society of London, London. Google Scholar

  6. The Geology of New Guinea - Free download as PDF File (.pdf), Text File (.txt) or read online for free. By Hugh L. Davies

  7. 20 de ene. de 2016 · 12 Citations. Explore all metrics. Abstract. We developed a probabilistic seismic hazard map of Papua New Guinea expressed in terms of peak ground acceleration with return period of 475 years. The calculations were performed for bedrock site conditions (Vs30 = 760 m/s).