Results 211 to 220 of about 18,722 (235)
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Complexity of the Oligocene meridional motion of the Philippine Sea Plate
GeologyAbstract The kinematic reconstruction of the Philippine Sea Plate (PSP) holds significant importance in elucidating the Australia–SE Asia collision and the Pacific Plate subduction. Previous studies suggested an overall northward motion of the PSP since its inception, but this first-order kinematic model cannot account for the observed ...
Wei Liu +6 more
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Paleomagnetic data from the Philippine Sea Plate and their tectonic significance
Journal of Geophysical Research: Solid Earth, 1991New paleomagnetic data from Guam and Saipan have been obtained and are used, in conjunction with previously published results from around the Philippine Sea plate, to interpret the origin and history of the Philippine Sea plate. A lower Miocene direction (I=3.5°, D=54.5°, a95=17.4°, k=20.3) and a middle Oligocene direction (I=5.3°, D=68.4°, a95=12.8 ...
Roger B. Haston, M. Fuller
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Cenozoic motion of the Philippine Sea Plate: Palaeomagnetic evidence from eastern Indonesia
Tectonics, 1995The history of motion of the Philippine Sea Plate is poorly known because it is isolated from the oceanic ridge system. Interpretation of palaeomagnetic results from the plate has been controversial because declination data have been obtained only from the eastern margin where subduction‐related tectonic processes may have caused local rather than ...
Hall, R, Ali, JR, Anderson, CD
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International Geology Review, 2006
The Cretaceous Rapu-Rapu Ophiolite Complex is a dismembered marginal basin ophiolite formed at an intermediate to fast spreading center. Limited subduction is manifested by the crystallization of pyroxene before plagioclase in the layered ultramafic cumulates.
Zhou, MF +3 more
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The Cretaceous Rapu-Rapu Ophiolite Complex is a dismembered marginal basin ophiolite formed at an intermediate to fast spreading center. Limited subduction is manifested by the crystallization of pyroxene before plagioclase in the layered ultramafic cumulates.
Zhou, MF +3 more
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Evidence for Early Cretaceous oceanic crust trapped in the Philippine Sea Plate
Earth and Planetary Science Letters, 2000The Huatung Basin is a small oceanic basin located east of Taiwan. Previous age estimates from magnetic lineationstudies indicated an Eocene age for the basin, and formation from the Central Basin Spreading Center of the WestPhilippine Basin during the last phase of spreading in Middle Eocene.
Deschamps, A. +4 more
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Receiver Function Image of the Subducting Philippine Sea Plate
2018We 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.
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Tectonics of the southern tip of the Parece Vela Basin, Philippine Sea Plate
Tectonophysics, 2009We report new geophysical and petrological data collected at the southern tip of the Parece Vela Basin in the Philippine Sea. The Parece Vela Basin, which was formed as a backarc basin behind proto Mariana arc-trench system from late Oligocene to middle Miocene, provides us a good opportunity to study the nature of successive backarc basin formations ...
Kyoko Okino +6 more
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Tectonophysics, 1995
Abstract The boundary between the Philippine Sea (PHS) and Eurasian (EUR) plates, which is presently seismically quiescent, is delineated on the basis of seismological data from the Kanto-Tokai (K-T) district during the period from January 1980 to April 1993.
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Abstract The boundary between the Philippine Sea (PHS) and Eurasian (EUR) plates, which is presently seismically quiescent, is delineated on the basis of seismological data from the Kanto-Tokai (K-T) district during the period from January 1980 to April 1993.
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The Philippine Sea Plate: Magnetism and reconstructions
1995Robert Hall +3 more
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Slab interactions in 3-D subduction settings: The Philippine Sea Plate region
Earth and Planetary Science Letters, 2018Adam F Holt +2 more
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