地质作用是一种长期复杂的作用过程,一个老矿床的形成常常要经过几亿或几十亿年的演化过程。而人们只能看到作用的结果,看不到它发展的全部过程,所以容易把多成因的矿床看成是简单一次形成的,这样就人为地把长期复杂的成矿过程给简单化了。近十多年来根据大量生产实践资料进行的综合研究,以及同位素地质、矿物包体研究,成岩成矿的模拟实验 Geological action is a long and complex process. The formation of an old deposit often goes through hundreds of millions or billions of years of evolution. People can only see the result of the action and can not see the whole process of its development. Therefore, it is easy to regard the multi-genesis deposit as a simple one-time formation, thus artificially simplifying the long-term complex ore-forming process. In the recent ten years, a comprehensive study based on a large number of production practice materials, as well as isotope geology, mineral inclusions, diagenetic mineralization simulation experiments