Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events-Reference-Cited by-同舟云学术

Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events

Published:2007-01-26 Issue:5811 Volume:315 Page:503-506
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Ito Yoshihiro¹,Obara Kazushige¹,Shiomi Katsuhiko¹,Sekine Shutaro¹,Hirose Hitoshi¹

Affiliation:

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

Abstract

We report on the very-low-frequency earthquakes occurring in the transition zone of the subducting plate interface along the Nankai subduction zone in southwest Japan. Seismic waves generated by very-low-frequency earthquakes with seismic moment magnitudes of 3.1 to 3.5 predominantly show a long period of about 20 seconds. The seismicity of very-low-frequency earthquakes accompanies and migrates with the activity of deep low-frequency tremors and slow slip events. The coincidence of these three phenomena improves the detection and characterization of slow earthquakes, which are thought to increase the stress on updip megathrust earthquake rupture zones.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference26 articles.

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4. Non-volcanic deep low-frequency tremors accompanying slow slips in the southwest Japan subduction zone

5. Thermal constraints on the seismogenic portion of the southwestern Japan subduction thrust

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