Gravity and geoid anomalies of the Philippine Sea: Evidence on the depth of compensation for the negative residual water depth anomaly [PDF]
A negative free-air gravity anomaly which occurs in the central part of the Philippine Sea was examined to determine the distribution and nature of possible regional mass excesses or deficiencies. Geoid anomalies from GEOS-3 observation were positive.
Bowin, C.
core +1 more source
Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma [PDF]
The configuration and kinematics of continental deformation and its marginal plate tectonics on the Earth's surface are intrinsic manifestations of plate-mantle coupling.
Gurnis, Michael +3 more
core
Kimberlite eruptions driven by slab flux and subduction angle. [PDF]
Mather BR +4 more
europepmc +1 more source
Estimation of the depth of origin of fluids using noble gases in the surface sediments of submarine mud volcanoes off Tanegashima Island. [PDF]
Mitsutome Y +5 more
europepmc +1 more source
Seismic potential associated with subduction in the northwestern United States [PDF]
Despite good evidence of present-day convergence of the Juan de Fuca and North American plates, there has been remarkably little historical seismic activity along the shallow part of the Juan de Fuca subduction zone.
Heaton, Thomas H., Kanamori, Hiroo
core
(WESTPAC) The Japan Trench, Japan Sea, Ryukyu Trench and Phillippine Sea
航海番号: KH-88-4 ; 航海日程: September 22 - Octorber 31 ...
openaire
3D Seismic Tomography Imaging of Taiwan Substructure [PDF]
Taiwan has a high rate of crustal deformation and a strong seismic activity. Taiwan is located on the convergent boundary between the Eurasian and the Philippine Sea plates.
Diah Ningrum, Susi Anggraini +1 more
core
Subducting volcaniclastic-rich upper crust supplies fluids for shallow megathrust and slow slip. [PDF]
Gase AC +11 more
europepmc +1 more source
Biased geodetic inference on asperity distribution on a subducted plate interface: a quantitative study [PDF]
core +1 more source

