Migrating tremors illuminate complex deformation beneath the seismogenic San Andreas fault
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature08755.pdf
Reference30 articles.
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2. Ide, S., Shelly, D. R. & Beroza, G. C. Mechanism of deep low frequency earthquakes: further evidence that deep non-volcanic tremor is generated by shear slip on the plate interface. Geophys. Res. Lett. 34 L03308 10.1029/2006GL028890 (2007)
3. Wech, A. G. & Creager, K. C. Cascadia tremor polarization evidence for plate interface slip. Geophys. Res. Lett. 34 L22306 10.1029/2007GL031167 (2007)
4. Shelly, D. R. et al. Precise location of San Andreas fault tremors near Cholame, California using seismometer clusters: slip on the deep extension of the fault? Geophys. Res. Lett. 36 L01303 10.1029/2008GL036367 (2009)
5. Nadeau, R. M. & Dolenc, D. Nonvolcanic tremors deep beneath the San Andreas fault. Science 307, 389, 10.1126/science.1107142 (2005); published online 9 December 2004.
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