Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
Laboratory Earthquakes: The Sub-Rayleigh-to-Supershear Rupture Transition
Kaiwen Xia,1,2Ares J. Rosakis,2Hiroo Kanamori1*
We report on the experimental observation of spontaneously nucleatedsupershear rupture and on the visualization of sub-Rayleightosupershearrupture transitions in frictionally held interfaces. The laboratoryexperiments mimic natural earthquakes. The results suggest thatunder certain conditions supershear rupture propagation canbe facilitated during large earthquake events.
1 Seismological Laboratory, MC 252-21, California Institute of Technology (Caltech), Pasadena, CA 91125, USA. 2 Graduate Aeronautical Laboratories, MC 105-50, Caltech, Pasadena, CA 91125, USA.
* To whom correspondence should be addressed. E-mail: hiroo{at}gps.caltech.edu
The editors suggest the following Related Resources on Science sites:
In Science Magazine
PERSPECTIVES
Mitiyasu Ohnaka (19 March 2004) Science303 (5665), 1788.
[DOI: 10.1126/science.1095765] |Summary »|Full Text »|PDF »
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
TeraShake2: Spontaneous Rupture Simulations of Mw 7.7 Earthquakes on the Southern San Andreas Fault.
K. B. Olsen, S. M. Day, J. B. Minster, Y. Cui, A. Chourasia, D. Okaya, P. Maechling, and T. Jordan (2008)
Bulletin of the Seismological Society of America
98, 1162-1185
|Abstract »|Full Text »|PDF »
A Unified Source Model for the 1906 San Francisco Earthquake.
S. G. Song, G. C. Beroza, and P. Segall (2008)
Bulletin of the Seismological Society of America
98, 823-831
|Abstract »|Full Text »|PDF »
Dynamic fibre sliding along debonded, frictional interfaces.