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贵州汞矿已有六百余年的开采历史。明朝洪武年间已生产,清朝开采尚盛,均用“火爆”和“手凿”法。1902年英法水银公司大量开采,1938年开始由伪资源委员会经营。1949年解放后,矿山获得了新生。空场采矿法沿革至今。一、矿床主要地质条件矿床产于寒武系中下统的C_1~3、C_2~3、C_2~5、C_2~7等矿层。中统以C_2~3层为主、C_2~8层次之。矿床倾角与地层一致,一般为7～10°,矿体赋存于矽化白云岩或矽化灰岩中,一般f=8～12。近矿围岩蚀变广泛,矽化与成矿密切,尤其是微石英蚀变体几乎同矿体大小一致,围岩稳固。
Guizhou mercury mine has more than 600 years of mining history. The Ming Dynasty Hongwu years have been produced, the Qing Dynasty mining Sheng, are “hot” and “chisel” method. In 1902, the British-French Mercury Company was mined extensively and was started in 1938 by the Pseudo-Resource Commission. After the liberation in 1949, the mine was reborn. Opencast mining law has so far. First, the main geological conditions Deposits occur in the Lower Cambrian C_1-3, C_2-3, C_2-5, C_2-7 ore deposits. Central to C_2 ~ 3-based, C_2 ~ 8 levels. The dip of the deposit is consistent with that of the strata, generally 7-10 °. Ore bodies occur in siliceous dolomite or silicified limestone, generally with f = 8-12. Nearly the ore wall rocks extensively alteration, silicification and mineralization are close, especially the microlithographic alteration body is almost the same with ore body size, the surrounding rock is firm.