Progress in seismic methodology and ambitious large‐scale seismic projects are enabling
high‐resolution imaging of the continental crust. The ability to constrain interpretations of …

Crustal anisotropy beneath 71 broadband seismic stations situated at the eastern Tibetan
Plateau and the Sichuan Basin is investigated based on the sinusoidal moveout of P-to-S …

Syncontractional extension is prominent in present-day Tibet, but its origin remains
vigorously debated. Several deep-seated geodynamic processes (eg, Indian underthrusting …

The fast orientation and magnitude of crustal azimuthal anisotropy beneath the southeastern
Tibetan Plateau and adjacent areas are measured by analyzing the sinusoidal moveout of …

The H‐κ method (Zhu & Kanamori, 2000, https://doi. org/10.1029/1999JB900322) has been
widely used to estimate the crustal thickness (H) and the ratio of P to S velocities (VP/VS …

Shear wave splitting parameters obtained along a linear array of 23 stations deployed in
western Tibet during a two-year period from 2011 to 2013 demonstrate strong and …

The lower crustal flow model has become an interesting proposal to describe the growth and
expansion of eastern Tibet. To date, however, the geophysical results are not definitive due …

Rocks in the continental crust are long lived and have the potential to record a wide span of
tectonic history in rock fabric. Map** rock fabric in situ at depth requires the application of …

Two types of surface wave anisotropy are observed regularly by seismologists but are only
rarely interpreted jointly: apparent radial anisotropy, which is the difference in propagation …

Seismic azimuthal anisotropy beneath the transitional region between the southeastern
Tibetan Plateau and the Indochina Peninsula, an area in which the fast orientation of mantle …