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5. THE ORIGIN OF DOUBLE HIGH CONDUCTIVITY LAYERS IN THE CRUST OF SOUTHERN TIBET AND ITS GEODYNAMIC

THE ORIGIN OF DOUBLE HIGH CONDUCTIVITY LAYERS IN THE CRUST OF SOUTHERN TIBET AND ITS GEODYNAMIC

来源 :地学前缘 | 被引量 : 0次 | 上传用户：ConchConch

【摘 要】

：

Geoelectrical investigations in Tibetan Plateau show that there are two high conductivity layers (HCLs) in the crust of southern Tibetan Plateau. The first HCL is at a depth of 15～20km, and the second

【出 处】

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地学前缘

【发表日期】

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2000年S1期

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Geoelectrical investigations in Tibetan Plateau show that there are two high conductivity layers (HCLs) in the crust of southern Tibetan Plateau. The first HCL is at a depth of 15～20km, and the second at 45～60km. In the central region of the Plateau, s

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