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- W2389831363 abstract "A new MT study was conducted along the profile EHS3D-3(Xiachayu of Tibet-Qingshuihe of Qinghai)in 2007.The preferred 2-D model suggests that:1)the upper crust consists of separated resistive blocks;2)in mid-lower crust there is an extensive conductor beneath Lhasa block and Qiangtang terrain respectively due to aqueous fluids and/or partial melts and are inferred to as crustal flow channels at depth of Tiebtan Plateau;3)Yarlun-Zangbo and Bangonghu-Nujiang sutures are indicated by two conductive layers dipping to the north;4)Jinshajiang Fault might be a fracture belt of upper crust that was thinned and destructed by the upwelling of the hot/conductive body at depth." @default.
- W2389831363 created "2016-06-24" @default.
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- W2389831363 date "2010-01-01" @default.
- W2389831363 modified "2023-09-23" @default.
- W2389831363 title "THE ELECTRICAL CONDUCTIVITY STRUCTURE OF THE EASTERN TIBETAN PLATEAU AND ITS TECTONIC IMPLICATIONS" @default.
- W2389831363 hasPublicationYear "2010" @default.
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