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[HTML][HTML] Plate tectonic cross-roads: Reconstructing the Panthalassa-Neotethys Junction Region from Philippine Sea Plate and Australasian oceans and orogens
SHA van de Lagemaat, DJJ van Hinsbergen - Gondwana Research, 2024 - Elsevier
The plate tectonic history of the Junction Region, which separated the Panthalassa and
Tethys realms, is notoriously challenging to reconstruct. The region has been dominated by …
Tethys realms, is notoriously challenging to reconstruct. The region has been dominated by …
The role of accommodation zones and transfer zones in the regional segmentation of extended terranes
JE Faulds, RJ Varga - 1998 - pubs.geoscienceworld.org
All normal-fault systems must terminate both along and orthogonal to strike. As many as four
terminations may be associated with a single culmination. Most normalfault systems …
terminations may be associated with a single culmination. Most normalfault systems …
Pliocene eclogite exhumation at plate tectonic rates in eastern Papua New Guinea
As lithospheric plates are subducted, rocks are metamorphosed under high-pressure and
ultrahigh-pressure conditions to produce eclogites and eclogite facies metamorphic rocks …
ultrahigh-pressure conditions to produce eclogites and eclogite facies metamorphic rocks …
Blueschists, eclogites, and subduction zone tectonics: Insights from a review of Late Miocene blueschists and eclogites, and related young high-pressure metamorphic …
T Ota, Y Kaneko - Gondwana Research, 2010 - Elsevier
In this paper, Late Miocene blueschist and eclogite belts, including the world's youngest
blueschist belt in Timor–Tanimbar Island chain, eastern Indonesia, and the world's youngest …
blueschist belt in Timor–Tanimbar Island chain, eastern Indonesia, and the world's youngest …
Contrasting styles of (U) HP rock exhumation along the Cenozoic Adria‐Europe plate boundary (Western Alps, Calabria, Corsica)
Since the first discovery of ultrahigh pressure (UHP) rocks 30 years ago in the Western Alps,
the mechanisms for exhumation of (U) HP terranes worldwide are still debated. In the …
the mechanisms for exhumation of (U) HP terranes worldwide are still debated. In the …
Diapiric exhumation of Earth's youngest (UHP) eclogites in the gneiss domes of the D'Entrecasteaux Islands, Papua New Guinea
The Woodlark Rift in Papua New Guinea hosts the world's youngest (2–8Ma) eclogite-facies
rocks and extensional deformation has played a key role in exhuming these (U) HP rocks at …
rocks and extensional deformation has played a key role in exhuming these (U) HP rocks at …
Divergence in subduction zones and exhumation of high pressure rocks (Eocene Western Alps)
Exhumation of high-pressure rocks has long remained a controversial issue in the Earth
sciences. In this article, we analyze the tectono-metamorphic, stratigraphic and plate-motion …
sciences. In this article, we analyze the tectono-metamorphic, stratigraphic and plate-motion …
Shallow dips of normal faults during rapid extension: Earthquakes in the Woodlark‐D'Entrecasteaux rift system, Papua New Guinea
GA Abers, CZ Mutter, J Fang - Journal of Geophysical …, 1997 - Wiley Online Library
Earthquakes in the Woodlark‐D'Entrecasteaux rift system reveal changes in fault geometry
along strike, as extension progresses from continental to oceanic modes. In one segment …
along strike, as extension progresses from continental to oceanic modes. In one segment …
Transient fluvial incision and active surface uplift in the Woodlark Rift of eastern Papua New Guinea
Abstract The Woodlark Rift of southeastern Papua New Guinea is among the fastest
evolving plate boundaries on Earth. Rapid extension led to formation of metamorphic core …
evolving plate boundaries on Earth. Rapid extension led to formation of metamorphic core …
Extensional detachment faulting and core-complex formation in the southern Barberton granite–greenstone terrain, South Africa: evidence for a 3.2 Ga orogenic …
The Barberton greenstone belt in South Africa is an Early-to Mid-Archaean, very low-grade
metamorphic supracrustal belt that is bordered in the south by a mid-to lower crustal gneiss …
metamorphic supracrustal belt that is bordered in the south by a mid-to lower crustal gneiss …