Ide S, Shiomi K, Mochizuki K, Tonegawa T, Kimura G (2010) Split Philippine Sea plate beneath Japan. Geophys Res Let 37:L21304. https://doi.org/10.1029/ 2010gl044585Ide S., Shiomi K., Mochizuki K., Tonegawa T., Kimura G. (2010) Split Philippine Sea plate beneath Japan . Geophys....
The proto-Philippine Sea Plate (pPSP) has been proposed by several authors to account for the origin of the Mesozoic supra-subduction ophiolites along the Philippine archipelago. In this paper, a comprehensive review of the ophiolites in the eastern portion of the Philippines is undertaken. Availa...
They affirm that the basin belongs to a different plate than WPB, the Taiwan Sea Plate. This plate would have formed in two different spreading episodes between 51 and 15 Ma, but its youngest portion is considered to have already been subducted beneath the Ryukyu Trench, explaining why only ...
Tectonic map and location of the seismic lines. The characteristic seafloor topography of the Philippine Sea plate on the left and position of the seismic lines across the Kyushu-Palau Ridge (KPR) on theright. An 8600 in.3(132L) tuned airgun array was shot alongred,black,andwhite lines, ...
There are also two low-velocity bodies with relatively high VP/VS ratios of 1.80–1.90 in the mantle wedge above the oceanic crust of the Philippine Sea plate. We speculate that the westernmost of these two low-velocity bodies consists of 20% partially serpentinized peridotite, continuous ...
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We compiled the most relevant data acquired throughout the Philippine Sea Plate (PSP) from the early expeditions to the most recent. We also analyzed the various explanatory models in light of this updated dataset. The following main conclusions are disc
We propose that the entire area north of the Sorong Fault in east Indonesia has always been part of the Philippine Sea Plate and that the whole plate has rotated clockwise in a discontinuous manner by approximately 90掳 since the early Eocene. The new data from north of the Sorong Fault ...
We construct receiver function (RF) image using onshore and offshore observatories located around the Kii Peninsula, southwest Japan, to investigate fluid distribution along the subducting Philippine Sea Plate. We calculate RFs at offshore sites using the inverse water-layer filter method. Resultant ...
The Sibuyan Sea branch is 350 km long and is presently active. It is more obvious on seismic and aeromagnetic data than the northern part of the known Philippine fault and thus may have accommodated more motion. We have made a preliminary evaluation of the total slip on the Sibuyan Sea ...