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文章详细研究庚村和黄双岭萤石矿的同位素分析结果，得出如下主要结论：成矿溶液来源于当地中生代大气降水；Ｓｒ，Ｂａ，Ｃａ来源于强蚀变的围岩；矿液中存在有ＨＦ和ＳｉＦ４。成矿过程氢、硫同位素出现交换动力学效应；庚村和黄双岭萤石矿的成矿年龄分别接近８４Ｍａ和１０７Ｍａ。
In this paper, the isotope analysis results of Gengcun and Huangshilingling fluorite ore are studied in detail. The main conclusions are as follows: the ore-forming solution is derived from the Mesozoic regional precipitation; Sr, Ba and Ca are derived from strong altered rock; HF and SiF4. The exchange kinetics of hydrogen and sulfur isotopes occurred in the ore-forming process, and the mineralization ages of Gengcun and Huangshilingling fluorite were close to 84Ma and 107Ma, respectively.