成矿作用 metallogenesis
- 摘要本文提出了构造成矿作用动力学研究的递增应力流变学方法。
An incremental stress rheology model is developed to study the dynamics of tectonic mineralization. - 成岩成矿作用是在总体挤压背景体制下的局部拉张环境下进行的。
And the authors found that magmatism and mineralization took place in the local tensional tectonic background within whole compressional one. - 文中还介绍了层状岩体中典型矿床的成矿作用与岩浆演化过程的成因联系。
Finally, a review is made on the genetic relationships between mineralization and magma evolution and the associated characteristic of ore systems.
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