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 used ambient noise data recorded by the NECESSArray, a portable seismic array
deployed in Northeast China, to construct Rayleigh-wave phase velocity dispersion curves …

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 …

Abstract The three-dimensional (3-D) electrical structure of the upper-mantle was used to
examine the deep origins of and relationship among the Cenozoic volcanoes located in …

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 …

We construct a new 3-D shear wave speed model of the crust and the uppermost mantle
beneath Northeast China using the ambient noise adjoint tomography method. Without …

In order to better understand the deep subduction geometry of the Pacific plate and genesis
of intraplate volcanism in northeast China (NE China), we computed a total of 45,505 …

Heat flow data are essential for understanding lithospheric dynamics. As a petroliferous
basin, a large number of boreholes have been drilled during hydrocarbon exploration and …

We present a new 3‐DS wave velocity model of the northeast (NE) China from the joint
inversion of the Rayleigh wave ellipticity and phase velocity at 8–40 s periods. Rayleigh …