Slow Earthquakes Linked Along Dip in the Nankai Subduction Zone-Reference-Cited by-同舟云学术

Slow Earthquakes Linked Along Dip in the Nankai Subduction Zone

Published:2010-12-10 Issue:6010 Volume:330 Page:1502-1502
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Hirose Hitoshi¹,Asano Youichi¹,Obara Kazushige¹²,Kimura Takeshi¹,Matsuzawa Takanori¹,Tanaka Sachiko¹,Maeda Takuto²³

Affiliation:

1. National Research Institute for Earth Science and Disaster Prevention, 3-1 Tennodai, Tsukuba, Ibaraki 305-0006, Japan.

2. Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo, Tokyo 113-0032, Japan.

3. Center for Integrated Disaster Information Research, Interfaculty Initiative in Information Studies, University of Tokyo, 1-1-1 Yayoi, Bunkyo, Tokyo 113-0032, Japan.

Abstract

Three types of temporally linked slow earthquakes may limit nearby buildup of stress.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference9 articles.

1. Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan

2. Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip

3. Episodic slow slip events accompanied by non-volcanic tremors in southwest Japan subduction zone

4. Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events

5. Coseismic slip resolution along a plate boundary megathrust: The Nankai Trough, southwest Japan

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