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当代对地质作用发展特点的认识存在着多种不同的观点，但总结各家的观点，可划分为两种对立的认识：一种认为地质作用过程是渐进的，具有连续性（演化）特点；而另一种则认为地质作用（包括成矿作用）的过程及现象具有断续性（灾变性）特点．然而，对某些成矿省及大矿区的地质
There are many different viewpoints on the contemporary understanding of the characteristics of the development of geology. However, to sum up the opinions of different quarters can be divided into two kinds of contradictions: one is that the geological process is gradual and has continuity (evolution) characteristics; The other is that the geological processes (including metallogenic processes) and the phenomenon of intermittent (catastrophic) characteristics. However, the geology of some metallogenic provinces and large mining areas