云南易门狮子山铜矿床围岩蚀变岩相与矿石组构特征研究

摘要

云南省易门狮子山铜矿床为昆阳裂谷典型的沉积-改造型铜矿床之一.矿床深部铜矿化与围岩蚀变有关,碳酸岩化与铜矿化关系密切.硅质白云岩类型铜矿体,矿石构造以脉状构造、浸染状构造为主；飘带矿矿石构造以层状构造为主.白云岩型铜矿中金属颗粒较细,为斑铜矿和黄铜矿；板岩型铜矿中金属颗粒较粗,为黄铜矿和黄铁矿.矿石化学成分具有高Si、Ca、Mg的特点,落雪组与鹅头厂组接触部位是重要的找矿地段.%Shizishan copper deposit,Yimeng,Yunnan is one of the typical sedimentary-reformed copper deposit in Kunyang rift valley.The Cu mineralization at the deep part of the deposit is relative to wall rock alteration,the carbonation has close relations with Cu mineralization.The ores in siliceous dolomite type copper ore body are mainly of vein structure,disseminated structure; the ribbon ore is mainly of layer structure.The mineral particle in dolomite type copper ore is finer,which is bornite and copper pyrites; the mineral particle in slate type copper ore is coarser,which is copper pyrites and pyrite.The chemical composition of ore has the features of high Si,Ca and Mg,the important prospecting area is the contact zone of Luoxue and Etouchang formations.