结果显示上部地壳结构总体上横向比较均匀，纵向分层明显。
The results show that the upper crustal structure is relatively well-distributed laterally and obviously by layers vertically.
岩石圈具有温度高、强度低和强烈流变分层等特征，且下地壳表现为韧性流动变形。
The lithosphere beneath this area is associated with high temperature, low strength and intensive rheological stratification, and the lower crust is characterized by ductile flow deformation.
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