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湘西钨锑金矿床主要分布于雪峰隆起之前寒武系浅变质岩系中。不同元素（矿物）组合的金矿床具有一系列特征性的成矿地质标志。
The tungsten-antimony-gold deposits in western Hunan are mainly distributed in the Cambrian shallow metamorphic rocks before the Xuefeng Uplift. The gold deposits with different element (mineral) combinations have a series of characteristic metallogenic geological signs.