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黑山梁钨钼矿床,位于甘肃北山北部,是近年在甘肃北山地区新发现的矿床。矿床位于哈萨克斯坦板块的黄山—红石山—路井晚古生代陆内裂谷带北缘,处于红石山—黑鹰山断裂带中,钨钼矿化分布在扫子山组2段中的构造裂隙中,矿区圈出钨矿体148个、钼矿体4个,大致呈NEE向似层状、脉状分布,矿床的成因类型可能属中高温热液型。
Heishanliang tungsten-molybdenum deposit, located in the northern part of Beishan, Gansu Province, is a newly discovered deposit in the Beishan area of Gansu in recent years. The deposit is located in the northern margin of the Late Paleozoic intracontinental rift zone of the Huangshan-Hongshishan-Passage of Kazakhstan Plateau, and is located in the Hongshishan-Heying fault zone. Tungsten and molybdenum mineralization is located in the structural fractures in the second member of the Swezishan Formation In the mining area, there are 148 tungsten ore bodies and 4 molybdenum ore bodies encircled in a roughly NEE-like pattern with vein-like distribution. The genetic type of the deposit may be of medium-high temperature hydrothermal type.