【摘 要】
：
Magnetotelluric(MT)surveys in the past decades have revealed that high-conductivity layers(0.01-1 S/m)widely exist in the mid-lower crust of Tibet plateau[1].
【机 构】
：
State Key Laboratory of Geological Processes and Mineral Resources,Wuhan 430074
【出 处】
：
第26届国际高压科学技术大会、第8届亚洲高压科技学术会议暨第19届中国高压科学技术会议(The 26th Interna
论文部分内容阅读
Magnetotelluric(MT)surveys in the past decades have revealed that high-conductivity layers(0.01-1 S/m)widely exist in the mid-lower crust of Tibet plateau[1].
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