本文为国家攀登专项（编号 SSER1112）,国土资源部项目（编号 9501112 ，95011020402,95011050302)和国家自然科学基金项目（编号 49772155）资助。
- 中国地质大学，北京，100083
- China University of Geosciences, Beijing,100083
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本文提出3个大地构造单元中火成岩构造组合及其所应的岩石圈—软流圈系统的状态，着重讨论了岩浆作用与深部壳幔过程对成矿作用的约束，简要讨论了它们的环境效应。提出研究岩石圈—软流圈动力学的演化趋势对中国大陆未来预测的重要性。
In this paper, three types of igneous petrotectonic assemblage s in t hree tec tonic settings, and their corresponding lithosphere—asthenosphere systems are p ut out. Disc uss ion emphatically on the constraints of the magmatism and deep crust—mantle proc e sses to the metallogenesis, and briefly on the environmental effect has been made. The significance of study on the evolution trend of the lithosphere-a sthenosphere system for the prediction of the China continent in the future is a lso discussed.
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邓晋福,罗照华,赵海玲,赵国春,李凯明.1999.岩浆作用、深部壳幔过程与资源-环境效应[J].地质论评,45(7):21-25,[DOI].
Deng Jinfu, Luo Zhaohua, Zhao Hailing, Zhao Guochun, Li Kaiming.1999. Magmatism, Deep Crust- Mantle Processes and Mineral Resources-Environment Effects[J]. Geological Review,45(7):21-25.
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