Repeating earthquakes, or repeaters, are identical in location and geometry but occur at
different times. They appear to represent recurring seismic energy release from distinct …

Repeating earthquakes (repeaters) that rupture the same fault area (patch) are interpreted to
be caused by repeated accumulation and release of stress on the seismic patch in a …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

Identification of repeating earthquakes (repeaters) usually depends on waveform similarity
expressed as the corresponding cross‐correlation coefficient (CC) above a prescribed …

We investigate the feasibility of using the dynamic time war** (DTW) technique as an
alternative to windowed cross correlation (WCC) for an indirect measure to quantify both the …

Repeating earthquakes (REs) rupture the same fault patches at different times allowing
temporal variations in the mechanical behavior of specific areas of the fault to be …

Repeating large earthquakes (M≥ 7), waveforms for which are nearly identical, have been
identified only on the Mexican subduction thrust near Acapulco. These earthquakes …

The Acapulco earthquake of 2021 broke a segment of the southeast Guerrero seismic gap
along the Mexican subduction thrust. The rupture initiated offshore Acapulco (16.770° N …

We investigated spatiotemporal change in the interplate seismic activity following the 2011
Tohoku‐oki earthquake (M9. 0) in the region where interseismic interplate coupling was …

Abstract The Mendocino Triple Junction (MTJ), at the northern terminus of the San Andreas
Fault system, is an actively deforming plate boundary region with poorly constrained …