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Published Online October 21, 2004
Science DOI: 10.1126/science.1103961

Reports

Submitted on August 11, 2004
Accepted on October 7, 2004

Earth Tides Can Trigger Shallow Thrust Fault Earthquakes

Elizabeth S. Cochran 1*, John E. Vidale 1, Sachiko Tanaka 2

1 Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, USA.
2 Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Miyagi 980-8578, Japan; Present address: National Research Institute for Earth Science and Disaster Prevention (NIED), Tsukuba-shi, Ibaraki-ken 305, Japan.

* To whom correspondence should be addressed.
Elizabeth S. Cochran , E-mail: cochran{at}moho.ess.ucla.edu

We show a correlation between the occurrence of shallow, thrust earthquakes and the occurrence of the strongest tides. The rate of earthquakes varies from the background rate by a factor of three with the tidal stress. The highest correlation is found when we assume a coefficient of friction of µ = 0.4 for the crust, although we see good correlation for µ between 0.2 and 0.6. Our results quantify the effect of applied stress on earthquake triggering, a key factor in understanding earthquake nucleation and cascades whereby one earthquake triggers others.


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