We present a new crustal thickness map of the Chinese mainland and adjacent areas based
on a compilation of previously published data. More than 1900 estimates of crustal thickness …

The southeastern (SE) margin of the Tibetan Plateau is a channel of the eastward esca**
material flow of the Tibetan Plateau. In order to fully understand the complex lithosphere …

This study, via combined analysis of geophysical and geochemical data, reveals a
lithospheric architecture characterized by crust–mantle decoupling and vertical heat-flow …

We determined a new 3‐DP‐wave velocity model of the upper mantle beneath eastern Tibet
using 112,613 high‐quality arrival‐time data collected from teleseismic seismograms …

Continental China consists of a complex amalgamation of geotectonic units and has
experienced strong and widespread tectonic deformation since the Mesozoic. To …

We present a new anisotropic tomographic model of the uppermost mantle around eastern
Tibet using Pn traveltime data from a newly deployed temporary seismic array and recent …

We analysed a large amount of teleseismic receiver function data recorded by 172
broadband stations in the NE Tibetan plateau and its surrounding areas to investigate the …

The continuous convergence between the Indian and Eurasian plates caused massive
lithospheric deformation in the Tibetan Plateau and led to excessive crustal material …

Broadband and long-period magnetotelluric (MT) data were used to obtain a continuous
image of the lithospheric electrical conductivity structure across the southeastern Tibetan …

The big mantle wedge (BMW) model was originally proposed to explain the origin of the
intraplate Changbaishan volcano in NE China where the subducting Pacific slab becomes …