Abstract The East Asian continent records a complex geologic and tectonic history that
involved the amalgamation of several small-to medium-sized blocks from Laurasia or …

Mechanisms for uplift and deformation of the Tibetan Plateau remain vigorously debated;
hypotheses include stepwise growth, distributed thickening, and crustal channel flow, each …

Azimuthal seismic anisotropy, the dependence of seismic wave speeds on propagation
azimuth, is largely due to fabrics within the Earth's crust and mantle, produced by …

The uplift of the Tibetan Plateau in the Cenozoic has greatly affected the tectonics in Asia.
But the evolution of the plateau is still unclear. The northeastern Tibetan Plateau is under …

We use a multi-station stacking method to analyze receiver function data recorded by a large-
scale dense seismic array covering the northeastern (NE) margin of the Tibetan plateau and …

In this study, we obtain a three‐dimensional (3‐D) high resolution seismic anisotropy model
of NE Tibet using ambient noise double beamforming (DBF) tomography with ChinArray …

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 …

We used teleseismic data recorded by a permanent seismic network in Yunnan, SE Tibet,
and measured the interstation Rayleigh wave phase velocity between 10 and 60 s. A two …

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 …