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- W2375927424 abstract "The resistivity model of central-north Tibet was obtained by 2D nonlinear conjugate gradients inversion with the data from Wudaoliang-Lvcaoshan magnetotelluric deep sounding profile,which consisted of partial sites from line 600 and all sites from line 2100.The features of the main faults beneath central-north Tibet were deduced according to this model as well as regional gravity,aero-magnetic and geological survey.The research results suggest that,there are sixteen faults,named F1 to F16 beneath central-north Tibet.Moreover,F1(Julushankecuo-Nangqian fault belt) and F9(Wulanwulahu-Yushu fault belt) are the northern edge of Jinshajiang suture,and the border between Songpan-Ganzi-Kekexili block and Qiangtang-Tanggula block.Kunlun fault zone consists of F4,F10 to F12.F4(Animaqin faults belt)is the border between Songpan-Ganzi-Kekexili block in the south and Kunlun-Qaidam block in the north.The northern edge fault zone of Qaidam basin consists of F6,F13 to F16,furthermore,F6 dips to south and penetrated the crust,F13 to F16 are a series of thrust faults dipping to north oppositely." @default.
- W2375927424 created "2016-06-24" @default.
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- W2375927424 date "2012-01-01" @default.
- W2375927424 modified "2023-10-04" @default.
- W2375927424 title "Electrical features of the main faults beneath Northern Tibetan Plateau" @default.
- W2375927424 hasPublicationYear "2012" @default.
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