赣南盘古山黑钨矿——辉铋矿石英脉矿床以规模大、品位高、矿化带稳定而著称。矿脉产于上泥盆统浅变质砂板岩中,矿体产状严格受一系列近E——W向“X”型裂隙控制。按矿脉产出状态分为南、中、北三组 Gansu Pangushan wolframite - bismuth ore vein pulse deposit to large-scale, high grade, well-known mineralized belt. The veins were produced in the upper Devonian metamorphic sand slate and the ore bodies were strictly controlled by a series of near E - W fractures. By the state of the vein is divided into South, Central and North three groups