A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion
Using data from more than 2000 seismic stations from multiple networks arrayed throughout
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
China (CEArray, China Array, NECESS, PASSCAL, GSN) and surrounding regions (Korean …
[HTML][HTML] 利用面波频散与接收函数联合反演青藏高原东南缘地壳上地幔速度结构
郑晨， 丁志峰， 宋晓东 - 地球物理学报, 2016 - html.rhhz.net
青藏高原东南缘对于青藏高原的隆升, 增厚和物质逃逸等问题有着重要的研究价值.
本文对研究区内布设的大型流动地震台阵的观测记录进行处理, 联合反演面波频散与接收函数 …
本文对研究区内布设的大型流动地震台阵的观测记录进行处理, 联合反演面波频散与接收函数 …
A synoptic view of the distribution and connectivity of the mid‐crustal low velocity zone beneath Tibet
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 …
more than 600 stations in and around Tibet, Rayleigh wave phase velocity maps are …
The structure of the crust and uppermost mantle beneath South China from ambient noise and earthquake tomography
Two years of continuous recordings of ambient seismic noise observed at 354 stations in
South China from 2009 to 2010 are used to estimate Rayleigh wave group and phase …
South China from 2009 to 2010 are used to estimate Rayleigh wave group and phase …
A unified map of Moho depth and Vp/Vs ratio of continental China by receiver function analysis
Continental China consists of a complex amalgamation of geotectonic units and has
experienced strong and widespread tectonic deformation since the Mesozoic. To …
experienced strong and widespread tectonic deformation since the Mesozoic. To …
Seismic evidence of on-going sublithosphere upper mantle convection for intra-plate volcanism in Northeast China
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 …
inversion of phase velocity dispersion curves at 6–140 s periods from ambient noise …
[HTML][HTML] 2021年5月21日云南漾濞MS6.4地震震区地壳结构特征与孕震背景
李大虎， 丁志峰， 吴萍萍， 刘韶， 邓菲， 张旭， 赵航 - 地球物理学报, 2021 - html.rhhz.net
本文基于" 中国地震科学台阵探测——南北地震带南段" 密集布设的流动地震台阵和川滇区域
数字测震台网等共计634 个台站所记录的观测资料, 先采用地震体波层析成像(TOMO3D) …
数字测震台网等共计634 个台站所记录的观测资料, 先采用地震体波层析成像(TOMO3D) …
An upper-mantle S-wave velocity model for East Asia from Rayleigh wave tomography
Y Li, Q Wu, J Pan, F Zhang, D Yu - Earth and Planetary Science Letters, 2013 - Elsevier
We present a new shear velocity model of the upper mantle beneath the East Asia region
derived by inverting Rayleigh wave group velocity measurements between 10 and 145 s …
derived by inverting Rayleigh wave group velocity measurements between 10 and 145 s …
Crust and uppermost mantle beneath the North China Craton, northeastern China, and the Sea of Japan from ambient noise tomography
A 3‐D shear velocity model of the crust and uppermost mantle to a depth of 100 km is
presented beneath the North China Craton (NCC), northeastern China, the Korean …
presented beneath the North China Craton (NCC), northeastern China, the Korean …
Crustal radial anisotropy across eastern Tibet and the western Yangtze craton
Phase velocities across eastern Tibet and surrounding regions are mapped using Rayleigh
(8–65 s) and Love (8–44 s) wave ambient noise tomography based on data from more than …
(8–65 s) and Love (8–44 s) wave ambient noise tomography based on data from more than …