一、概述我矿属前震旦纪沉积——变质热液含钴铜矿床。矿体呈似层状、串珠状和音叉状产出,金属矿物主要为黄铜矿、黄铁矿、磁黄铁矿,钴呈类质同像存在于上述矿物中,尤以黄铁矿含钻最丰富。矿体边界不清,依取样分析方可圈定铜、钻或复合矿体。开采对象以铜为主,铜矿体厚度多在5～20米之间。 First, an overview of mine is pre-Sinian sedimentary - metamorphic hydrothermal cobalt-bearing copper deposits. Ore bodies appear to be layered, beaded and fork-shaped output, the main metal minerals are chalcopyrite, pyrite, pyrrhotite, cobalt was similar to the existence of similar minerals, especially pyrite Drill the most abundant. Ore boundary is not clear, according to the sample analysis can be delineated copper, diamond or composite ore body. Copper-based mining targets, copper ore thickness more than 5 to 20 meters.