在昆仑山脉与雅鲁藏布缝合带之间，向东的流动便形成上部地壳的滑脱构造。
Between the Kunlun fault and Yarlung Zangbo suture the eastward flow resulted in the formation of detachments in the upper crust.
两缝合带之间没发现壳内高导层，地壳表现为相对完整的高阻体；
There is no high conductivity layer between the two plate suture zones, on the other hand the crust is an integrated high resistivity body.
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