Crust and mantle in these two areas are coupled as complicated crust mantle transitional zone consisting of multiple laminae with alternate high and low velocities, totaling 20 km in thickness.

 
  • 海原地震區和巴顏喀拉地塊與柴達木地塊結合帶莫霍面具有明顯的活動(dòng)跡象;殼幔耦合為復雜的高、低速相間的多層殼幔過(guò)渡帶;總厚度達到20多千米.
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