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Lateral Inhomogeneity of Basement Layer in Three Gorges Region of Changjiang River (Yangtze River)
引用本文:Bian Yinju,Hu Hongxiang,and Gao ShiyuInstitute of Geophysics,SSB,Beijing 100081,China. Lateral Inhomogeneity of Basement Layer in Three Gorges Region of Changjiang River (Yangtze River)[J]. 中国地震研究, 1997, 0(4)
作者姓名:Bian Yinju  Hu Hongxiang  and Gao ShiyuInstitute of Geophysics  SSB  Beijing 100081  China
作者单位:Bian Yinju,Hu Hongxiang,and Gao ShiyuInstitute of Geophysics,SSB,Beijing 100081,China
基金项目:This project was sponsored by the Joint Earthquake Science Foundation (93084), China. Contribution No. 96A0095, Institute of Geophysics, SSB, China
摘    要:Seismic tomography from the Pg wave data along the non-longitudinal profile in the Three Gorges Region is presented in this paper.The seismic tomography method,and the acquisition and analysis of seismic travel time are broadly outlined.The tomography of basement reveals a great amount of significant information and shows that the low-velocity zone is due to the lithologic difference and the fault fracture zone.It also demonstrates that there exist three high-velocity zones with v>6.4 km/s at the basement; the largest of zones which strikes north-south is located at the southwestern side of Huangling Anticlinorium and extends into the anticlinorium northward.The other two high-velocity zones are,respectively,situated at the eastern side of the anticlinorium and the western side of the profile.The high-velocity zones are inferred to originate from the upwelling of material with high-velocity from deep crust.


Lateral Inhomogeneity of Basement Layer in Three Gorges Region of Changjiang River (Yangtze River)
Bian Yinju,Hu Hongxiang,and Gao ShiyuInstitute of Geophysics,SSB,Beijing ,China. Lateral Inhomogeneity of Basement Layer in Three Gorges Region of Changjiang River (Yangtze River)[J]. Earthquake Research in China, 1997, 0(4)
Authors:Bian Yinju  Hu Hongxiang  and Gao ShiyuInstitute of Geophysics  SSB  Beijing   China
Affiliation:Bian Yinju,Hu Hongxiang,and Gao ShiyuInstitute of Geophysics,SSB,Beijing 100081,China
Abstract:Seismic tomography from the Pg wave data along the non-longitudinal profile in the Three Gorges Region is presented in this paper.The seismic tomography method,and the acquisition and analysis of seismic travel time are broadly outlined.The tomography of basement reveals a great amount of significant information and shows that the low-velocity zone is due to the lithologic difference and the fault fracture zone.It also demonstrates that there exist three high-velocity zones with v>6.4 km/s at the basement; the largest of zones which strikes north-south is located at the southwestern side of Huangling Anticlinorium and extends into the anticlinorium northward.The other two high-velocity zones are,respectively,situated at the eastern side of the anticlinorium and the western side of the profile.The high-velocity zones are inferred to originate from the upwelling of material with high-velocity from deep crust.
Keywords:Three Gorges region   seismic tomography   basement layer   Huangling anti-clinorium.
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