Our models and understanding of the dynamics of earthquake rupture are based largely on
estimates of earthquake source parameters, such as stress drop and radiated seismic …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

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 …

We present a novel method for measuring the fluctuating basal normal and shear stresses of
debris flows by using along‐channel seismic recordings. Our method couples a simple …

We calculate rupture directivity and velocity for earthquakes in three well‐recorded
repeating sequences (2001–2016) on the San Andreas Fault at Parkfield using P waves …

The static stress drop of an earthquake is an indicator of the stress state of a specific fault
before rupture initiation. The stress state is primarily controlled by the ambient stress field …

The aim of this study is to investigate the directivity effects of~ 250 aftershocks (magnitudes 3–
5.5) of the Mw 6.1 2009 L'Aquila earthquake (central Italy). To this end, we estimate the …

Spectral analysis is widely used to estimate and refine earthquake source parameters such
as source radius, seismic moment, and stress drop. This study aims to quantify the precision …

Abstract On Gofar Transform Fault on the East Pacific Rise, the largest earthquakes (6.0≤
MW≤ 6.2) have repeatedly ruptured the same portion of the fault, while intervening fault …