Mineralisation associated with fault, vein and shear zone systems can be related to
processes that operated when those systems were active. Despite the complexity of …

How fault geometry controls the rupture propagation and segmentation of a strike-slip event
is an open question. Deciphering the relationship between the geometric fault complexity …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

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

Large [moment magnitude (M w)≥ 7] continental earthquakes often generate complex,
multifault ruptures linked by enigmatic zones of distributed deformation. Here, we report the …

Surface rupture in the 2019 Ridgecrest, California, earthquake sequence occurred along
two orthogonal cross faults and includes dominantly left‐lateral and northeast‐striking …

Abstract The 2008 M w 7.9 Wenchuan earthquake ruptured an imbricate thrust system in the
Longmen Shan range, which forms the eastern boundary of the Tibetan Plateau. We use …

Abstract The 1872 Owens Valley earthquake is the third largest known historical earthquake
in California. Relatively sparse field data and a complex rupture trace, however, inhibited …

Distributions of coseismic slip help illuminate many properties of earthquakes, including fault
geometry, stress changes, frictional properties, and potential future hazard. Slip inversions …

Observations of recent earthquake surface ruptures show that ground deformations include
a localized component occurring on faults, and an off‐fault component affecting the …