Template matching has proven to be an effective method for seismic event detection, but is
biased toward identifying events similar to previously known events, and thus is ineffective at …

Low-frequency earthquakes (LFEs) are seismic phenomena with the shortest timescale
among various slow earthquakes observed on broad-band timescales. To understand the …

Slow earthquakes are now commonly found to display a wide range of durations, moments,
and slip and propagation speeds. But not all types of slow earthquakes have been …

Numerous efforts have been made to interpret the intriguing characteristics of low-frequency
earthquakes (LFEs) and tectonic tremor in relation to regular earthquakes. At subduction …

Since the 1960s, we have observed creep events along the central San Andreas Fault.
Despite this, we still do not know (1) when they occur,(2) where they occur,(3) how they grow …