Migrating low-frequency tremors observed at shallow subduction interface

Tuesday, July 7, 2015 - 07:20 in Earth & Climate

A University of Tokyo research group has discovered slow-moving low-frequency tremors which occur at the shallow subduction plate boundary in Hyuga-nada, off east Kyushu. This indicates the possibility that the plate boundary in the vicinity of the Nankai Trough is slipping episodically and slowly (over days or weeks) without inducing a strong seismic wave.

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