By data classification and geological analysis based upon the P-wave velocity values acquired from geophysical synthesized profiles, the authors divide the lithospheric crust of South China into upper,middle,and lower crust( the P-wave velocity of upper crust (< 6.
利用从地球物理综合剖面上取得的P波速度数据,进行数据处理归类,按照VP速度值的大小,结合地质分析,将华南地区岩石圈地壳划分出上、中、下地壳(上地壳P波速度<6。
However,the extensive Mesozoic metamorphism and magmatism have been weakly related to lithosphere delamination.
岩石圈拆沉是碰撞造山带物质成分调整和构造演化的重要方式之一。
