Variability in earthquake stress drop and apparent stress
Author:
Affiliation:
1. Department of Geophysics; Stanford University; Stanford; California; USA
2. Department of Earth and Planetary Science; University of Tokyo; Tokyo; Japan
3. Departamento de Física; Universidad de los Andes; Bogota; Colombia
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1106/2011GL046698/2011GL046698.pdf
Reference25 articles.
1. Earthquake source scaling relationships from −1 to 5 ML using seismograms recorded at 2.5-km depth;Abercrombie;J. Geophys. Res.,1995
2. Scaling law of earthquake source time-function;Aki;Geophys. J. R. Astron. Soc.,1972
3. Global variations of stress drop for moderate to large earthquakes;Allmann;J. Geophys. Res.,2009
4. Radiated seismic energy from coda measurements and no scaling in apparent stress with seismic moment;Baltay;J. Geophys. Res.,2010
5. A spectral theory for circular seismic sources; simple estimated of source dimension, dynamic stress drop, and radiated seismic energy;Boatwright;Bull. Seismol. Soc. Am.,1980
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