论文部分内容阅读
岩石圈不连续是岩石圈块体间的构造薄弱带,也是岩石圈单元和深部成矿单元划分的重要界线;本文以华北地台为例,阐述岩石圈不连续的概念,初步探讨了岩石圈不连续在大陆成矿作用过程中的作用,并讨论了岩石圈不连续的识别标志。
The discontinuity of lithosphere is the tectonic weak zone between lithosphere blocks and also an important boundary for the division of lithospheric units and deep metallogenic units. Taking North China platform as an example, the paper expounds the concept of lithosphere discontinuity, The role of discontinuities in the mineralization in the mainland and the identification of discontinuous lithosphere are discussed.