Improved 3‐D P Wave Azimuthal Anisotropy Structure Beneath the Tokyo Metropolitan Area, Japan: New Interpretations of the Dual Subduction System Revealed by Seismic Anisotropy-Reference-Cited by-同舟云学术

Improved 3‐D P Wave Azimuthal Anisotropy Structure Beneath the Tokyo Metropolitan Area, Japan: New Interpretations of the Dual Subduction System Revealed by Seismic Anisotropy

Published:2021-03 Issue:3 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Ishise Motoko¹^ORCID,Kato Aitaro¹^ORCID,Sakai Shin'ichi¹²³,Nakagawa Shigeki¹^ORCID,Hirata Naoshi¹³^ORCID

Affiliation:

1. Earthquake Research Institute The University of Tokyo Bunkyo City Japan

2. Interfaculty Initiative in Information Studies The University of Tokyo Bunkyo City Japan

3. Research Center for Enhancing Metropolitan Resilience National Research Institute for Earth Science and Disaster Resilience Tsukuba Japan

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB021194

Reference43 articles.

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5. A three‐dimensional velocity structure and configuration of the Philippine Sea slab beneath Kanto district, Japan estimated by double‐difference tomography (in Japanese with English abstract), Zisin;Hirose F.;Journal of the Seismological Society of Japan,2008

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