Northeastern Tibet is still in the primary stage of tectonic deformation and is the key area for
studying the lateral expansion of the Tibetan plateau. In particular, the existence of lower …

The northeastern margin of Tibet is of key importance in understanding the uplift and
expansion of Tibetan Plateau. In this research, we perform Rayleigh wave tomography from …

We present high‐resolution tomographic images of isotropic P wave velocity and azimuthal
anisotropy in the crust and uppermost mantle beneath NE Tibet by jointly inverting 62,339 …

Abstract The cratonic Sichuan Basin is located east of the Tibetan Plateau, and is
surrounded by mountains that have undergone complex deformation and uplift since the …

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 …

We use receiver functions calculated for data collected by the INDEPTH‐IV seismic array to
image the three‐dimensional geometry of the crustal and upper mantle velocity …

The eastern region of the Tibetan Plateau and surrounding regions have gentle to moderate
topographic gradients, contrasting the steep margins in northern and southern Tibet. The …

Constraining variations of lithospheric structure and deformation across southeastern Tibet
and the surrounding region are crucial for understanding the lateral growth of the plateau …

A dense linear array of 38 broadband seismograph stations was deployed to traverse the
northeastern margin of Tibetan plateau (NE Tibet). Shear wave splitting measurements …

Abstract The Tibetan Plateau is produced by the continental-continental collision between
the India and Eurasian plates as well as the subsequent convergence. It has become a …