The Manila Trench - West Taiwan Foldbelt: a flipped subduction zone
The Manila Trench-West Taiwan Foldbelt is an anomalous west-facing island arc segment of the western Pacific. It is postulated to be a young, east-dipping subduction zone which flipped in Pliocene time from a former west-dipping position on the east side
Editor Geological Society of Malaysia
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Evolutionary Histories of Camellia japonica and Camellia rusticana. [PDF]
Abe H +9 more
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Palaeolithic voyage for invisible islands beyond the horizon. [PDF]
Kaifu Y, Kuo TH, Kubota Y, Jan S.
europepmc +1 more source
Novel mapping approach for coastal boulders using deep learning. [PDF]
Yamada K +3 more
europepmc +1 more source
Onset of double subduction controls plate motion reorganisation. [PDF]
Zhang K, Liao J, Gerya T.
europepmc +1 more source
Role of warm subduction in the seismological properties of the forearc mantle: An example from southwest Japan. [PDF]
Lee C, Kim Y.
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Neotectonics in Southern Ryukyu arc by means of paleostress analysis [PDF]
Paleostress estimation is essential in understanding the tectonics of the Southern Ryukyu arc. We have used Multiple inverse method (Yamaji, 2000) and Ginkgo method (Yamaji, 2003) to detect paleostress from the fault-slip data collected in the Southern ...
林, 大五郎 +2 more
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Arc magma formation through the fluid-fluxed mélange melting in subduction zones. [PDF]
Zhang W +4 more
europepmc +1 more source
Millennial scale maximum intensities of typhoon and storm wave in the northwestern Pacific Ocean inferred from storm deposited reef boulders. [PDF]
Minamidate K +7 more
europepmc +1 more source
Phylogeography of Ryukyu insular cicadas: Extensive vicariance by island isolation vs accidental dispersal by super typhoon. [PDF]
Osozawa S +3 more
europepmc +1 more source

