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前言 武山铜矿分为南、北两个矿带,其中南矿带为矽卡岩型铜矿床,矿石类型简单。北矿带为含铜黄铁矿床,矿石类型较复杂,除含铜黄铁矿外,尚有含铜高岑土和含铜角砾岩。三者在负120米中段以上分别占77.68％、17.76％和4.56％,在负40米中段以上分别占80％、13％和7％。 本带有用矿物主要是胶状黄铁矿、黄铁矿、兰辉铜矿、辉铜矿、铜兰,其次为黄铜矿、斑铜矿。少量赤铜矿、黑铜矿、孔雀石,脉石矿物大部份为石英,其次为粘土矿物(多水高岑石、高岑石、水云母、蒙脱石),再就是碳酸盐矿物,其他脉石矿物含量很少。
Foreword Wushan Copper Mine is divided into two northern and southern ore belts, of which the southern ore belt is a skarn type copper deposit with simple ore type. The northern ore belt is a copper-bearing pyrite deposit, and the type of ore is rather complicated. In addition to the copper-bearing pyrite, copper-bearing high-concentration soil and copper-bearing breccia are still present. The three sectors accounted for 77.68%, 17.76% and 4.56% respectively above the mid-120s, while 80%, 13% and 7% respectively above the mid-40s. The main minerals are colloidal pyrite, pyrite, Langhui copper, chalcopyrite, copper orchid, followed by chalcopyrite, bornite. A small amount of red copper, black copper, malachite, gangue minerals most of the quartz, followed by clay minerals (water high Cen Cen Stone, Cen Cen Stone, water mica, montmorillonite), then carbonate minerals , Other gangue mineral content is very small.