Low-velocity oceanic crust at the top of the Philippine Sea and Pacific plates beneath the Kanto region, central Japan, imaged by seismic tomography

Author:

Matsubara Makoto,Hayashi Hiroki,Obara Kazushige,Kasahara Keiji

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference33 articles.

1. The abundance of serpentinites in the oceanic crust;Christensen;J. Geol.,1972

2. Poisson's ratio and crustal seismology;Christensen;J. Geophys. Res.,1996

3. Structure and constitution of the lower oceanic crust;Christensen;Rev. Geophys.,1975

4. Subduction factory: 1. Theoretical mineralogy, densities, seismic wave speeds, and H2O contents;Hacker;J. Geophys. Res.,2003

5. Kanto-Tokai observation network of crustal activities— National Research Center for Disaster Prevention (in Japanese, with English abstract);Hamada;J. Seismol. Soc. Jpn.,1982

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