Physics
Scientist
Department of Geophysics, Stanford University, Stanford, California, USA
U.S. Geological Survey, Menlo Park, California, USA
Department of Earth and Planetary Science, University of California, Berkeley, California, USA
An autocorrelation method to detect low frequency earthquakes within tremor
Bridging the gap between seismically and geodetically detected slow earthquakes
Brittle and ductile friction and the physics of tectonic tremor
Deep low-frequency earthquakes in tremor localize to the plate interface in multiple subduction zones
Locating non-volcanic tremor along the San Andreas Fault using a multiple array source imaging technique
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