The southwestern edge of the Ryukyu subduction zone: A high Q mantle wedge-Reference-Cited by-同舟云学术

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The southwestern edge of the Ryukyu subduction zone: A high Q mantle wedge

Published:2012-06 Issue: Volume:335-336 Page:145-153
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Ko Yen-Ting,Kuo Ban-Yuan,Wang Kuo-Lung,Lin Shu-Chuan,Hung Shu-Huei

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference50 articles.

1. Shear wave velocity, seismic attenuation, and thermal structure of the continental upper mantle;Artemieva;Geophys. J. Int.,2004

2. Seismic anisotropy reveals focused mantle flow around the Calabrian slab (Southern Italy);Baccheschi;Geophys. Res. Lett.,2007

3. An inverted continental Moho and serpentinization of the forearc mantle;Bostock;Nature,2002

4. Dehydration and partial melting in subduction zones: constraints from U-series disequilibrium;Bourdon;J. Geophys. Res.,2003

5. Tomography of the western Ryukyu subduction zone and the serpentinization of the fore-arc mantle;Chou;J. Geophys. Res.,2009

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