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结合矿区野外工作和室内资料的综合整理,参考区域资料,将矿区构造划分为北东向、北北东向、北西向及北西西向等四个构造体系,提出了北东向构造带、北北东向带、北西向构造带及北西西向构造带的构造演化史。研究表明,区域上以北东向构造为主,萤石矿受北东向构造和北西西向构造带的控制。即北东向构造与北西西向构造是成矿的有利构造部位。
Combining the fieldwork and indoor data mining in the mining area, with reference to the regional data, the tectonic structures of the mining area are divided into four structures: NE, NE, NW and NWW. The North East structural belt Tectonic evolution of the Eastward, Northwestern and Northwestern-West tectonic belts. The study shows that the area is dominated by the NE structure and the fluorite ore is controlled by the NE structure and the NW-NW structure. That is, the NE-trending and NW-trending structures are favorable structural sites for metallogenesis.