Three-dimensional P-wave velocity structure beneath Central Japan: low-velocity bodies in the wedge portion of the upper mantle above high-velocity subducting plates-Reference-Cited by-同舟云学术

Three-dimensional P-wave velocity structure beneath Central Japan: low-velocity bodies in the wedge portion of the upper mantle above high-velocity subducting plates

Published:1989-06 Issue:1-2 Volume:163 Page:63-73
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Hirahara K.,Ikami A.,Ishida M.,Mikumo T.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference27 articles.

1. Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz;Aki;Phys. Earth Planet. Inter.,1980

2. Determination of three-dimensional velocity anomalies under a seismic array using first P arrival times from local earthquakes. 1. A homogeneous initial model;Aki;J. Geophys. Res.,1976

3. Crustal structure in the profile across central Japan as derived from explosion seismic observations;Aoki;J. Phys. Earth,1972

4. Shear wave polarization anisotropy in the upper mantle beneath Honshu Japan;Ando;J. Geophys. Res.,1983

5. Observations of shear-wave polarization anisotropy and low P-wave bodies: partially melted diapirs in the upper mantle;Ando;Abstr. 23rd Gen. Assem. IASPEI,1985

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