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自从1948年毕里宾提出关于地壳活动带成矿作用的重要概念以来,地槽区内生成矿作用的学说得到了发展.众所周知,这个学说的基本点可以归结为这样一种思想,即一定的岩浆岩及与其有关的金属矿床,产生于活动地槽转化为相对稳定的褶皱区的各个连续阶段之中.与此同时,斯塔里茨基等人开始了古地台成矿作用问题的研究.近年来,主要是由于舍格洛夫及卡尔波娃有关活化区成矿作用的著作,使古老地台与年青地台的成矿作用研究更加深入了,并对此产生了越来越大的兴趣.不仅如此,综合上面提到的以及其他成矿研究的成果,现在
The doctrine of generative mineralization in the trough area has been developed since Bribbin proposed an important concept of mineralization in the crustal activity zone in 1948. It is well known that the basic point of this doctrine can be attributed to the notion that a certain Magmatic rocks and their associated metallogenic deposits originate in successive stages of the active terrains transforms into relatively stable fold zones, while Stalitzki et al. Started the study of the mineralization of paleo-terraces In recent years, mainly due to the writings on the mineralization of the activated zone by Segalov and Karpova, the study on the mineralization of the ancient platform and the young platform has been further deepened and more and more Not only that, but also the results of other mineralization studies mentioned above and now