<div><p>The Owen Stanley Fault Zone (OSFZ) is the low-angle thrust boundary between the Australian and Woodlark plates. The eastern extension of the OSFZ links with the Woodlark Basin spreading centre. Recent tectonic models of eastern Papua depict the OSFZ boundary passing through the Mt Suckling district, with the Keveri Fault a key component. Gravity data clearly show that the OSFZ and the Papuan Ultramafic Belt (PUB) pass north of Mt Suckling. Tectonised mafic and ultramafic rocks of the Mt Suckling district, previously referred to the PUB, are reassigned to the Awariobo Range Complex (new name). Extensive pillow basalts previously referred to the middle Eocene part of the Kutu Volcanics at the top of the PUB sequence are, in the map ar...
There are four main phases in the diastrophic evolution of western Papua and New Guinea: (1) a Meso...
The island of New Guinea marks the northern extent of the Australian continental margin, where it li...
The present zircon fission track thermochronology study reveals Triassic to Pliocene source terrains...
The calculated extension (~111 km) across the Woodlark rift is incompatible with the > 130 km needed...
The Kukukuku Lobe is a complex uplift of Miocene sediments. This uplift basically represents the inv...
<p>Woodlark Island (Muyuw) is located in a tectonically complex region, one of the few places on Ear...
New Guinea forms the northern margin of the Australian Plate which is now characterised by a zone c...
textThe D'Entrecasteaux Island (DEI) gneiss domes are fault-bounded domes with ~2.5 km of relief exp...
© 2021 Luke George MahoneyThe Papuan Fold and Thrust Belt (PFTB) in Papua New Guinea (PNG), located ...
A shallow-dipping ductile mylonitic shear zone and concordant brittle detachment fault (Mai'iu fault...
SUMMARY: The sea floor around eastern New Guinea is divided into a number of deep basins, separated ...
The island of Papua New Guinea is the result of continent-arc collision that began building the isla...
This thesis aims to establish how the late Cenozoic oblique convergence of the Pacific- Caroline and...
Detailed stratigraphic and structural analysis has shown that tectonic development in the central Pa...
The ~750 km2 Dayman dome of the Late Cretaceous Suckling-Dayman massif, eastern Papua New Guinea, is...
There are four main phases in the diastrophic evolution of western Papua and New Guinea: (1) a Meso...
The island of New Guinea marks the northern extent of the Australian continental margin, where it li...
The present zircon fission track thermochronology study reveals Triassic to Pliocene source terrains...
The calculated extension (~111 km) across the Woodlark rift is incompatible with the > 130 km needed...
The Kukukuku Lobe is a complex uplift of Miocene sediments. This uplift basically represents the inv...
<p>Woodlark Island (Muyuw) is located in a tectonically complex region, one of the few places on Ear...
New Guinea forms the northern margin of the Australian Plate which is now characterised by a zone c...
textThe D'Entrecasteaux Island (DEI) gneiss domes are fault-bounded domes with ~2.5 km of relief exp...
© 2021 Luke George MahoneyThe Papuan Fold and Thrust Belt (PFTB) in Papua New Guinea (PNG), located ...
A shallow-dipping ductile mylonitic shear zone and concordant brittle detachment fault (Mai'iu fault...
SUMMARY: The sea floor around eastern New Guinea is divided into a number of deep basins, separated ...
The island of Papua New Guinea is the result of continent-arc collision that began building the isla...
This thesis aims to establish how the late Cenozoic oblique convergence of the Pacific- Caroline and...
Detailed stratigraphic and structural analysis has shown that tectonic development in the central Pa...
The ~750 km2 Dayman dome of the Late Cretaceous Suckling-Dayman massif, eastern Papua New Guinea, is...
There are four main phases in the diastrophic evolution of western Papua and New Guinea: (1) a Meso...
The island of New Guinea marks the northern extent of the Australian continental margin, where it li...
The present zircon fission track thermochronology study reveals Triassic to Pliocene source terrains...