The quantity and quality of satellite-geodetic measurements of tectonic deformation have
increased dramatically over the past two decades improving our ability to observe active …

Crustal faults usually have a fault core and surrounding regions of brittle damage, forming a
low-velocity zone (LVZ) in the immediate vicinity of the main slip interface. The LVZ may …

Coseismic surface deformation in large earthquakes is typically measured using field
map** and with a range of geodetic methods (eg, InSAR, lidar differencing, and GPS) …

Comparisons of observed surface displacements with geodetically inferred slip at depth in
six large (M w⩾ 7.1) strike-slip earthquakes reveal a correlation between the structural …

We present a method for estimating radar phase delays due to propagation through the
troposphere and the ionosphere based on the averaging of redundant interferograms that …

The trifurcation area of the San Jacinto fault zone has produced more than 10% of all
earthquakes in southern California since 2000, including the June 2016 M w (moment …

Earthquake source spectra contain fundamental information about the dynamics of
earthquake rupture. However, the inherent tradeoffs in separating source and path effects …

Mature strike‐slip faults are usually surrounded by a narrow zone of damaged rocks
characterized by low seismic wave velocities. Observations of earthquakes along such faults …

Hydrologic loads can stimulate seismicity in the Earth's crust. However, evidence for the
triggering of large earthquakes remains elusive. The southern San Andreas Fault (SSAF) in …

Observations of shallow fault creep reveal increasingly complex time‐dependent slip
histories that include quasi‐steady creep and triggered as well as spontaneous accelerated …