The Xiaojiang fault system (XJFS), located to the southeast of the Tibetan Plateau, has a
complicated tectonic history and is an ideal location to study the Tibetan Plateau in terms of …

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

The lithospheric architecture of the South China Block (SCB) is crucial to understanding the
formation and evolution of this distinctive and highly reworked continental lithosphere with …

Abstract The Permian Emeishan large igneous province (LIP) in Southwestern China is
recognized as a remnant of mantle plume activity. Its crust composition has a significant …

Abstract The Emeishan Large Igneous Province (ELIP) is located along southeastern margin
of the Tibetan Plateau, where long-wavelength crustal thickening and surface uplift have …

We obtained a panoptic view of the pattern of mantle flow in the “Big Mantle Wedge”
associated with the stagnation of the subducting Pacific slab. We applied a simultaneous …

Seismic anisotropy reveals that seismic wave velocity, amplitude, and other physical
properties show variations in different directions, which can be divided into lattice preferred …

The selected rotation angle and deconvolution time window during S‐wave receiver function
(SRF) calculations, and the final SRF quality control may introduce artificial interference …

Abstract The eastern Tibetan Plateau (TP) is crucial to the exploration of plateau outgrowth
mechanisms. Teleseismic attenuation may provide constraints on anelasticity in the …

The Cenozoic sediments are very thick in the southwest Tarim Basin and very thin in the
northwest, but what controls these variations is unclear. Here, we use two‐dimensional …