We investigated the upper mantle anisotropy beneath China by applying teleseismic shear wave splitting measurements at 119 seismic stations from CDSN and GSN/IRIS networks in China.The splitting observations are characterized by apparent diversity of anisotropy pattern in adjacent tectonic domains,i...06583-59
The Tien Shan is an intraplate mountain belt situated between two stable Precambrian continental blo...
This study presents a total of 12008 shear wave splitting measurements obtained using the reference-...
The vast majority of teleseismic XKS (including SKS, SKKS and PKS) shear wave splitting studies inte...
Seismic anisotropy in the mantle beneath mainland China was studied using data from the China Digita...
We measured shear wave splitting from SKS data recorded by the transcontinental NECESSArray in NE Ch...
S-waves converted from P-wave at different boundaries inside the earth, i.e., the Moho discontinuity...
[1] Northeast China is situated partly on the Sino‐Korean craton and partly on a portion of the Inne...
About 700 shear-wave splitting meausurements obtained at global and regional seismic stations in NE ...
[1] We have obtained velocity images of the uppermost mantle beneath China by performing tomographic...
Knowledge about seismic anisotropy can provide important insight into the deformation of the crust a...
The May 12, 2008 magnitude 7.9 Wenchuan earthquake occurred along the Longmenshan thrust fault, whic...
Global mantle convection significantly impacts the processes at Earth’s surface and has been used to...
We obtained shear wave splitting measurements from XKS (SKS and SKKS) phases recorded by the NECESSA...
The upper crustal anisotropy of Yunnan area, SE margin of Tibetan Plateau, is investigated by measur...
The Haiyuan fault is a large strike-slip fault in the northeastern (NE) margin of the Tibetan platea...
The Tien Shan is an intraplate mountain belt situated between two stable Precambrian continental blo...
This study presents a total of 12008 shear wave splitting measurements obtained using the reference-...
The vast majority of teleseismic XKS (including SKS, SKKS and PKS) shear wave splitting studies inte...
Seismic anisotropy in the mantle beneath mainland China was studied using data from the China Digita...
We measured shear wave splitting from SKS data recorded by the transcontinental NECESSArray in NE Ch...
S-waves converted from P-wave at different boundaries inside the earth, i.e., the Moho discontinuity...
[1] Northeast China is situated partly on the Sino‐Korean craton and partly on a portion of the Inne...
About 700 shear-wave splitting meausurements obtained at global and regional seismic stations in NE ...
[1] We have obtained velocity images of the uppermost mantle beneath China by performing tomographic...
Knowledge about seismic anisotropy can provide important insight into the deformation of the crust a...
The May 12, 2008 magnitude 7.9 Wenchuan earthquake occurred along the Longmenshan thrust fault, whic...
Global mantle convection significantly impacts the processes at Earth’s surface and has been used to...
We obtained shear wave splitting measurements from XKS (SKS and SKKS) phases recorded by the NECESSA...
The upper crustal anisotropy of Yunnan area, SE margin of Tibetan Plateau, is investigated by measur...
The Haiyuan fault is a large strike-slip fault in the northeastern (NE) margin of the Tibetan platea...
The Tien Shan is an intraplate mountain belt situated between two stable Precambrian continental blo...
This study presents a total of 12008 shear wave splitting measurements obtained using the reference-...
The vast majority of teleseismic XKS (including SKS, SKKS and PKS) shear wave splitting studies inte...
DOI
Add to ORKG