Can observations of earthquake scaling constrain slip weakening?
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/162/2/406/5961297/162-2-406.pdf
Reference118 articles.
1. Earthquake source scaling relationships from −1 to 5 using seismograms recorded at 2.5 km depth;Abercrombie;J. geophys. Res.,1995
2. Source parameters of small earthquakes recorded at 2.5 km depth, Cajon Pass, southern California: implications for earthquake scaling;Abercrombie;Geophys. Res. Lett.,1993
3. Insights on fault behavior from the seismic nucleation phase;Ampuero;EOS, Trans. Am. geophys. Un., Fall Meeting Suppl.,2002
4. Rupture velocity of plane strain shear cracks;Andrews;J. geophys. Res.,1976
5. Dynamic plane-strain shear rupture with a slip-weakening friction law calculated by a boundary integral method;Andrews;Bull. seism. Soc. Am.,1985
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