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今年二月我們在某銅矿用分散流进行普查打矿的试验工作,取得了一定的地質效果,証实了用分散流普查找矿是行之有效的找矿方法,它若与地质普查相結合必然得到完滿的找矿效果。現将此次所作的方法介绍于后。一、一般情况本区位于大地构造单元上的康滇地轴之南端,以元古代昆阳系为主,为中溫热液矿床,矿体賦存在扁(?)状白云岩中,矿物以黄銅矿为主,輝銅矿次之,氧化矿物則以孔雀石为主,呈细脈状和散点状。本区为高原侵蝕型地形,地形变化較大且陡峻,
In February this year, we conducted a census and mining operation on a copper mine with scattered flows and achieved some geological results. It is confirmed that the prospecting of ore deposits by means of generalized scattered flow exploration is an effective prospecting method. If it is compared with the geological survey phase Combination must be a complete prospecting effect. Now this method is introduced in the later. First, the general situation The area is located in the southern tectonic unit of the southern end of the Kang Dian axis to the Proterozoic Kunyang Department, as the mesothermal hydrothermal deposit, ore body exists flat (?) Shaped dolomite, the mineral brass Ore, followed by chalcocite, oxidized minerals are mainly malachite, was fine veins and scattered. This area is plateau-eroded terrain, the terrain changes greatly and steep,