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 …

Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …

Competing geodynamic models, such as rigid-block extrusion, continuous deformation, and
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …

We propose a method to invert surface wave dispersion data directly for 3-D variations of
shear wave speed, that is, without the intermediate step of phase or group velocity maps …

The uplift of the Tibetan Plateau in the Cenozoic has changed the tectonics of the whole
Asia and affected the climate and environment significantly. However, the mechanism of the …

We present a 3‐D radially anisotropic model of the crust and mantle beneath East Asia
down to 900 km depth. Adjoint tomography based on a spectral element method is applied …

Seismic tomography has provided key insight into Yellowstone's crustal magmatic system
that includes attempts to understand the melt distribution in the subsurface and the current …

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

Since the continental collision between the Indian and Eurasian plates began about 50 Ma
ago, southeastern Tibet (SET) has undergone complex tectonic deformation. In this study …

Shear-wave splitting provides insight into geodynamic processes such as lithospheric
deformation and upper mantle flow. This study presents shear wave splitting parameters …