Seismic tomography has been a vital tool in probing the Earth's internal structure and
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …

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

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 …

Based on 1–2 years of continuous observations of seismic ambient noise data obtained at
more than 600 stations in and around Tibet, Rayleigh wave phase velocity maps are …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

A 3-D crustal and upper mantle S-wave velocity model of NE China is constructed by
inversion of phase velocity dispersion curves at 6–140 s periods from ambient noise …

Ambient noise tomography (ANT) has recently become a popular tomography method to
study crustal structures thanks to its unique capability to extract short-period surface waves …

The factors that promote stability of Archean cratons are investigated from a combined
geodynamic, geological, and geophysical perspective in order to evaluate the relative …

Understanding the Mesozoic–Cenozoic tectonic evolution of the North China Craton (NCC)
and the NE Tibetan Plateau (TP) requires detailed knowledge of the lithospheric structure …

A high-resolution P-wave tomography of the crust and mantle down to 700km depth beneath
the Japan Islands is determined using a large number of high-quality arrival-time data from …