HelioWebUniversity of Papua New Guinea
flowchart
I[University of Papua New Guinea]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (14)"]
CA["Linked Collaborating Authors (0)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Papuan Ultramafic Belt (PUB) Ophiolite: Field Mapping, Petrology, Mineral chemistry, Geochemistry, Geochronology, And Experimental Studies Of The Metamorphic Sole
- Preliminary Modeling of Tsunami Waves Generated by the Earthquake of 9 September 2002 Offshore of Northern Papua New Guinea
- Preliminary results of field survey, 2002 PNG earthquake at Wewak
- Seismological Aspects of the 2002 Papua New Guinea and Andaman Earthquakes and Tsunamis
- Using Drowned Coral Reefs to Constrain Flexural Models for Lower Plate Subsidence History: the Huon Gulf, Papua New Guinea
- Velocity profiles and turbulent structure over the sand bed of the lower Strickland River, Papua New Guinea
- Decadal sediment accumulation rates on the floodplain of the Strickland River, Papua New Guinea
- Active source seismic experiment investigating the formation of the Ontong Java Plateau
- Thick lower crustal body constrained by a seismic experiment at the center of the Ontong Java Plateau
- Archaeological jade mystery solved using a 119-year-old rock collection specimen
- 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
- Evidence of Melt percolation and Mantle Wedge Deformation in the Marum Ophiolite (Papua New Guinea)
- Crustal thickness of the Ontong Java Plateau and deep reflections near the base of its crust
- Evidence of melting, melt percolation and deformation in a supra-subduction zone (Marum ophiolite complex - Papua New Guinea)