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湖南石门雄黄矿床受寒武系下统娄山关群白云岩和下奥陶统灰岩以及断裂构造的双重控制。构造控制了古岩溶的形成，岩溶控（成）矿特征明显。通过遥感、物化探资料解译，运用多元统计方法，圈定了８个远景区。
The Shimen-Huanghuang deposit in Hunan is controlled by the Loushanguan Group dolomite and the Lower Ordovician limestone under the Cambrian and the fault structure. Structure controls the formation of ancient karst, karst control (into) ore features obvious. Through the remote sensing, geophysical and geochemical data interpretation, the use of multivariate statistical methods, delineated 8 long-range area.