假孔雀石赋存于铜矿床氧化带,系铜矿石中不常见的氧化铜矿物,因其颜色与孔雀石相似,往往被人忽视。几年来我们在对铜录山铜矿氧化铜矿石的研究中,发现了该矿物,并对其性质、共生状态及可选性进行了研究。研究结果表明,假孔雀石为含铜磷酸盐,用硫化—黄药浮选法难以选别,但可在碱性介质中用油酸钠或羟肟酸直接浮选。 Fake malachite occurs in the oxidation zone of copper deposits, is not common in copper ores of copper oxide minerals, because of its color and malachite similar, often overlooked. In recent years, we have discovered this mineral in the study of Tonglushan copper mine copper oxide ore, and studied its nature, symbiotic state and its selectivity. The results show that the false malachite is a copper-containing phosphate, with sulfide - yellow flotation method is difficult to choose, but in alkaline medium with sodium oleate or hydroxamic acid direct flotation.