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Updated: Jul 2, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

Débil acoplamiento entre placas por montañas submarinas y repetición de M aproximadamente 7 terremotos

Kimihiro Mochizuki1, Tomoaki Yamada, Masanao Shinohara

  • 1Earthquake Research Institute, University of Tokyo, 1-1-1, Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan. kimi@eri.u-tokyo.ac.jp

Science (New York, N.Y.)
|August 30, 2008
PubMed
Resumen

Es posible que las montañas submarinas de subducción no fortalezcan el acoplamiento de la placa como se esperaba. Los datos sísmicos de la Fosa del Japón sugieren un acoplamiento débil sobre una montaña submarina subductora, que influye en las áreas de ruptura de terremotos.

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