Azimuthally-aligned shear-wave splitting is widely observed in the Earth's crust. The splitting
is diagnostic of some form of seismic anisotropy, although the cause of this anisotropy has …

Seismic shear-wave splitting is difficult to measure accurately because of the complexity of
the shear-wave signal. A variety of techniques have been developed for measuring time …

Measurements of the splitting or birefringence of seismic shear waves that have passed
through the Earth's mantle yield constraints on the strength and geometry of elastic …

We analyze temporal variations of seismic velocity along the Karadere-Düzce branch of the
north Anatolian fault using seismograms generated by repeating earthquake clusters in the …

We present tomographic images of crustal structures in the southern California plate-
boundary area, with a focus on the San Jacinto fault zone (SJFZ), based on double …

We deployed a dense linear array of 45 seismometers across and along the San Andreas
fault near Parkfield a week after the M 6.0 Parkfield earthquake on 28 September 2004 to …

We perform a systematic analysis of crustal anisotropy along and around the Karadere—
Düzce branch of the North Anatolian fault (NAF), which ruptured during the 1999 Mw 7.4 …

The Haiyuan fault is a large strike-slip fault in the northeastern (NE) margin of the Tibetan
plateau. Using new data recorded by a temporary seismic array, this study obtains crustal …

We analyse fault zone trapped waves, generated by∼ 500 small earthquakes, for high-
resolution imaging of the subsurface structure of the Coyote Creek, Clark Valley and Buck …

We perform comprehensive analyses of trapped waves and signals of damaged fault zone
rocks associated with time delays of body waves along the Parkfield section of the San …