地球化学省是区域岩石圈演化过程中形成的,是具有共同成因的、一定规模的地质单元的地球化学表现。
The geochemical province, formed in the course of regional lithospheric evolution, is characterized by geological units with common origin and certain sizes.
在岩石圈演化历史上,上述不同性质力源的相对强弱和作用方式,决定了岩石圈运动的性质及其驱动机制。
In evolution history of he lithosphere, the relative strength and acting way of the above forces determine the characteristics and driving mechanism of the lithosphere movement.
[6]杨承海。鲁西中生代高镁闪长岩的年代学和地球化学:对华北克拉通岩石圈演化的制约[D]。长春:吉林大学,2007。
YANG Cheng-hai. Chronology and Geochemistry of Mesozoic High-Mg Diorites in Western Shandong:Constraints of Lithospheric Evolution of the North China Craton[D]. Changchun:Jilin University, 2007.
应用推荐