To better understand the subsurface behavior of subducting slabs and their relation to the
tectonic evolution of the overriding plate, we conduct a full waveform inversion on a large …

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 …

This review discusses the major milestone results yielded by the regional seismological
studies of the deep structure of the Earth's crust and mantle beneath the Baikal rift since the …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

In this study, I present a high‐resolution 3‐D Vs model of the crust and uppermost mantle
beneath central Mongolia, based on seismic data recorded at the Central Mongolia Seismic …

The detailed images of the mantle transition zone (MTZ) give insights into the nature of
mantle upwelling from the deep Earth. We use receiver function to investigate the MTZ …

In this paper, the 3-D S-wave velocity structure of the crust and upper mantle in the Abaga
volcanic area of Inner Mongolia was inverted by using the surface-wave tomography …

Central Mongolia is marked by wide spread recent volcanism as well as significant
topographic relief even though it is far from any plate tectonic boundaries. The cause of the …

We present new high‐resolution Pn velocity and anisotropy models beneath Mongolia and
the adjacent regions by inverting 169,406 Pn arrivals. The data are selected from 786 …

We present tomographic models of frequency-dependent Lg and Sn attenuation in eastern
Mongolia using data from 228 local earthquakes that were recorded by 69 broad-band …