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

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 …

We have obtained a high resolution 3-D crustal and uppermost mantle velocity model of the
Ordos block and its surrounding areas by joint inversion of ambient noise tomography and …

Abstract The Tanlu Fault Zone (TLFZ) and Chifeng‐Kaiyuan Fault (CKF) serve as tectonic
boundaries between the North China Craton (NCC) and the Central Asian Orogenic Belt …

We present a 3‐D model of NE China by joint inversion of body and surface waves. The joint
inversion significantly improves the resolution at shallow depths compared with body wave …

In this study, we re-examined the crustal and uppermost mantle shear velocity structure
beneath Northeast China using the broadband ambient seismic noise data from several …

We present a 3D thermochemical model of the North China Craton (NCC) from the surface
down to 350 km by jointly inverting surface wave phase velocity data, geoid height, surface …

We determine robust 3-DP-wave anisotropic tomography of the crust and upper mantle
beneath NE China using high-quality traveltime data of local earthquakes and teleseismic …

We deployed a linear seismic array consisting of 50 broadband stations in the southern part
of the Great **ng'an orogenic belt to investigate seismic anisotropy in the Songliao Basin …

There exists much debate about origins of Cretaceous to present volcanism in northeast
(NE) China. Here we present high‐resolution seismic images of the upper mantle beneath …