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从地球物貭的运动与发展过程来认識成矿作用,有两个基本問題:一是原子的演变、形成、以及原子在地壳表层的存在形式;二是原子在自然空間和时間上的运动与分布,迁移与富集。其次,是研究原子的演变、形成、运动与地貭条件的联系。研究大区域成矿作用,一般都是从地貭条件着手,如成矿区域在地壳大型构造单元中的位置;区域內的岩浆岩种别;围岩特点;沉积环境和成矿深度等等。这些地貭条件可以影响地壳內某些元素的分散与集中,所以认識这些条件之間的联系,有可能检查地球物貭
There are two basic problems in understanding the mineralization process from the movement and development of the earth’s geology. One is the evolution and formation of atoms, and the existence of atoms in the surface layer of the earth’s crust. The other is that the atoms are in natural space and time Movement and distribution, migration and enrichment. Secondly, it is to study the relationship between the evolution, formation and movement of atoms and the conditions of the earth. Research on metallogenesis in large areas generally begins with the geomagnetic conditions, such as the location of metallogenic regions in large crustal tectonic units, the types of magmatic rocks in the area, the characteristics of the surrounding rocks, the sedimentary environment and the metallogenic depth, and so on. These terrestrial conditions can affect the dispersion and concentration of certain elements in the crust, so knowing the connection between these conditions makes it possible to examine geocenters