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断裂变动的发展问题,始终引起地质工作者的注意,因为它对岩浆岩和成矿的分布,特别是在再次活化区所起的作用是相当大的。同时,用传统的方法研究断裂的发展对露头好的和良好的地质环境是很有效的。但
The development of fracture variation has always attracted the attention of geologists because of its considerable contribution to the distribution of magmatic rocks and mineralization, especially in the area of reactivation. In the meantime, it is very effective to study the development of faults by the traditional method for outcroping good and good geological environment. but