Using data from more than 2000 seismic stations from multiple networks arrayed throughout China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean Seismic Network, F-Net, KNET), we perform ambient noise Rayleigh wave tomography across the entire region and earthquake tomography across parts of South China and Northeast China. We produce isotropic Rayleigh wave group and phase speed maps with uncertainty estimates from 8 to 50 s period across the entire region of study, and extend them to 70 s period where earthquake tomography is performed. Maps of azimuthal anisotropy are estimated simultaneously to minimize anisotropic bias in the isotropic maps, but are not discussed here. The 3D model is produced using a Bayesi...
The objective of this project is to use a combination of travel-time and surface wave tomography to ...
We present a new 3-D S wave velocity model of the northeast (NE) China from the joint inversion of t...
Seismic methods using natural earthquakes are commonly applied to investigate the velocity structure...
A 3-D shear velocity model of the crust and uppermost mantle to a depth of 100 km is presented benea...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
[1] We perform ambient noise tomography of China using data from the China National Seismic Network ...
This work is the mantle component of constructing the Seismological Reference Earth Model in South C...
We present the first-generation full-waveform tomographic model (SinoScope 1.0) for the crust-mantle...
Two years of continuous recordings of ambient seismic noise observed at 354 stations in South China ...
We present the first-generation full-waveform tomographic model (SinoScope 1.0) for the crust-mantle...
We present a new 3-D S wave velocity model of the northeast (NE) China from the joint inversion of t...
The objective of this project is to use a combination of travel-time and surface wave tomography to ...
We present a new 3-D S wave velocity model of the northeast (NE) China from the joint inversion of t...
Seismic methods using natural earthquakes are commonly applied to investigate the velocity structure...
A 3-D shear velocity model of the crust and uppermost mantle to a depth of 100 km is presented benea...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
We present a three-dimensional model of shear wave velocity for the upper mantle of China and the su...
[1] We perform ambient noise tomography of China using data from the China National Seismic Network ...
This work is the mantle component of constructing the Seismological Reference Earth Model in South C...
We present the first-generation full-waveform tomographic model (SinoScope 1.0) for the crust-mantle...
Two years of continuous recordings of ambient seismic noise observed at 354 stations in South China ...
We present the first-generation full-waveform tomographic model (SinoScope 1.0) for the crust-mantle...
We present a new 3-D S wave velocity model of the northeast (NE) China from the joint inversion of t...
The objective of this project is to use a combination of travel-time and surface wave tomography to ...
We present a new 3-D S wave velocity model of the northeast (NE) China from the joint inversion of t...
Seismic methods using natural earthquakes are commonly applied to investigate the velocity structure...