The structure and dynamics of the upper mantle control tectonics, seismicity, magmatism,
and the development of mineral deposits. Seismic tomography maps spatial variations in …

Mongolia, a major world-class site of Cenozoic intracontinental tectonics, provides a key
proxy for the long-term dynamics of Eurasia, but there has been considerable debate about …

A low-velocity layer atop the mantle transition zone has been extensively observed
worldwide. In subduction zones, this layer is widely explained as partial melting triggered by …

The mechanisms of surface uplift of Hangai Dome (> 2 km) and formation of Cenozoic
intraplate volcanism in central Mongolia remain vigorously debated. Here we directly …

We provide a comprehensive image of the mantle transition zone (MTZ) beneath
northeastern China by performing Variable Bin Radius Stacking of receiver functions. A …

The genesis of the Cenozoic intraplate volcanism in Central Mongolia, characterized by
sustained and low-volume eruptions remains debated due to the lack of a comprehensive …

In the eastern segment of the Central Asian Orogenic Belt (CAOB), there is widespread
volcanic magma activity. However, there is still considerable controversy over the formation …

Abstract The Mongolian Plateau in Central Asia is an intracontinental tectonic system far
from active plate boundaries. Despite its distance from these boundaries, the plateau is …

The upper mantle and the transition zone of the Baikal rift zone (BRZ) are studied. The
observations are analyzed from P-wave receiver functions. It is found that in the BRZ central …