As the western boundary of the Sichuan-Yunnan block (SYB), the Red River fault (RRF) is a
major fault that controls deep crustal movement and deformation in the southeast margin of …

Rheology of rocks controls the deformation of the Earth at various space-time scales, which
is crucial to understand the tectonic evolution of continental lithosphere. Researches of rock …

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 …

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 …

The northeastern Tibetan plateau margin is the current expansion border, where growth of
the plateau is ongoing. We analyze shear-wave splitting at ChinArray stations in the NE …

The collision of the South China Block and the North China Block and the eastward
extrusion of the Tibetan Plateau materials have caused complicated tectonic deformation …

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 …

The tectonic evolution and deformation process of the southeastern Tibetan Plateau has
been one of the focuses of the geoscience community in recent decades. However, the …

An azimuth‐dependent dispersion curve inversion (ADDCI) method is applied to Rayleigh
waves to extract 3D velocity and azimuthal anisotropy. The synthetic tests show that the …