Tiny intraplate earthquakes triggered by nearby episodic tremor and slip in Cascadia
Author:
Affiliation:
1. Department of Earth and Space Sciences; University of Washington; Box 351310; Seattle; Washington; 98195; USA
2. U.S. Geological Survey, Department of Earth and Space Sciences; University of Washington; Box 351310; Seattle; Washington; 98195; USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/gc/gc1106/2011GC003559/2011GC003559.pdf
Reference24 articles.
1. Deep low-frequency earthquakes in tremor localize to the plate interface in multiple subduction zones;Brown;Geophys. Res. Lett.,2009
2. Earth tides can trigger shallow thrust fault earthquakes;Cochran;Science,2004
3. Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone, New Zealand;Delahaye;Earth Planet. Sci.Lett.,2009
4. A silent slip event on the deeper Cascadia subduction interface;Dragert;Science,2001
5. Tremor bands sweep Cascadia;Ghosh;Geophys. Res. Lett.,2010
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