Sr, Nd, and Pb isotope compositions of hemipelagic sediment in the Shikoku Basin: Implications for sediment transport by the Kuroshio and Philippine Sea plate motion in the late Cenozoic

2015 ◽  
Vol 421 ◽  
pp. 47-57 ◽  
Author(s):  
Yu Saitoh ◽  
Tsuyoshi Ishikawa ◽  
Masaharu Tanimizu ◽  
Masafumi Murayama ◽  
Yurika Ujiie ◽  
...  
Keyword(s):  
Sediment Transport ◽  
Plate Motion ◽  
Philippine Sea Plate ◽  
Late Cenozoic ◽  
Pb Isotope ◽  
Philippine Sea ◽  
Shikoku Basin ◽  
Hemipelagic Sediment ◽  
The Kuroshio

Basin filling related to the Philippine Sea Plate motion in Beppu Bay, southwest Japan

2016 ◽  
Vol 117 ◽  
pp. 13-22 ◽  
Author(s):  
Keitaro Yamada ◽  
Keiji Takemura ◽  
Michinobu Kuwae ◽  
Ken Ikehara ◽  
Masanobu Yamamoto
Keyword(s):  
Plate Motion ◽  
Philippine Sea Plate ◽  
Southwest Japan ◽  
Philippine Sea

scholarly journals Philippine Sea Plate motion since the Eocene estimated from paleomagnetism of seafloor drill cores and gravity cores

2010 ◽  
Vol 62 (6) ◽  
pp. 495-502 ◽  
Author(s):  
Toshitsugu Yamazaki ◽  
Masaki Takahashi ◽  
Yasufumi Iryu ◽  
Tokiyuki Sato ◽  
Motoyoshi Oda ◽  
...  
Keyword(s):  
Plate Motion ◽  
Philippine Sea Plate ◽  
Philippine Sea ◽  
Drill Cores

Geodetic constraints on postseismic deformation following the 1990Ms7.8 Luzon earthquake and implications for Luzon tectonics and Philippine Sea plate motion

2001 ◽  
Vol 2 (9) ◽  
pp. n/a-n/a ◽  
Author(s):  
John Beavan ◽  
David Silcock ◽  
Michael Hamburger ◽  
Emmanuel Ramos ◽  
Catherine Thibault ◽  
...  
Keyword(s):  
Plate Motion ◽  
Philippine Sea Plate ◽  
Postseismic Deformation ◽  
Philippine Sea

scholarly journals North Luzon and the Philippine Sea Plate motion model: Insights following paleomagnetic, structural, and age-dating investigations

2007 ◽  
Vol 112 (B5) ◽  
Author(s):  
Karlo L. Queano ◽  
Jason R. Ali ◽  
John Milsom ◽  
Jonathan C. Aitchison ◽  
Manuel Pubellier
Keyword(s):  
Age Dating ◽  
Plate Motion ◽  
Philippine Sea Plate ◽  
Motion Model ◽  
Philippine Sea

Detection of Philippine Sea Plate Motion by very long baseline interferometry

1991 ◽  
Vol 18 (8) ◽  
pp. 1417-1419 ◽  
Author(s):  
Shigeru Matsuzaka ◽  
Mikio Tobita ◽  
Yoshiro Nakahori ◽  
Jun Amagai ◽  
Yuji Sugimoto
Keyword(s):  
Very Long Baseline Interferometry ◽  
Plate Motion ◽  
Philippine Sea Plate ◽  
Philippine Sea ◽  
Long Baseline

scholarly journals Rotation of the Philippine Sea plate inferred from paleomagnetism of oriented cores taken with an ROV-based coring apparatus

2021 ◽  
Vol 73 (1) ◽  
Author(s):  
Toshitsugu Yamazaki ◽  
Shun Chiyonobu ◽  
Osamu Ishizuka ◽  
Fumisato Tajima ◽  
Naoki Uto ◽  
...  
Keyword(s):  
Plate Motion ◽  
Philippine Sea Plate ◽  
Late Oligocene ◽  
Clockwise Rotation ◽  
Polar Wander ◽  
Philippine Sea ◽  
Apparent Polar Wander Path ◽  
Paleomagnetic Study ◽  
History Of ◽  
The Mean

AbstractReconstructing the history of Philippine Sea (PHS) plate motion is important for better understanding of the tectonics of the surrounding plates. It is generally considered that the PHS plate migrated northward since Eocene, but its rotation has not been constrained well; some reconstructions incorporated a large clockwise rotation but others did not. This is mainly because the difficulty of collecting oriented rocks from the mostly submerged PHS plate hindered establishing an apparent polar wander path. In this study, we conducted a paleomagnetic study of oriented cores taken using an ROV-based coring apparatus from the Hyuga Seamount on the northern part of the Kyushu-Palau Ridge, a remnant arc in the stable interior of the PHS plate. Stepwise thermal and alternating-field demagnetizations were applied to specimens taken successively from two ~ 30 cm long limestone cores of middle to late Oligocene age, and characteristic remanent magnetization directions could be isolated. Declination and inclination of D = 51.5° and I = 39.8°, respectively, were obtained as the mean of the two cores. The easterly-deflected declination means ~ 50° clockwise rotation of the PHS plate since middle to late Oligocene. In addition, ~ 5° latitudinal change of the site is estimated from the mean inclination. The result implies that the Kyushu-Palau Ridge was located to the southwest of the present position in middle to late Oligocene, and that PHS plate rotation as well as the Shikoku and Parece Vela Basin spreading contributed to the eastward migration of the Izu-Ogasawara (Bonin) Arc to the current position.

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