新疆康古尔塔格金矿床的副氯铜矿发现及其地质意义  

Paratacamite of Kanggu'ertage gold deposit in the Xinjiang Uygur Autonomous Region of China

作　　者：白开寅[1] 韩照信[1] 

机构地区：[1]长安大学成矿作用及其动力学开放实验室,陕西西安710054

出　　处：《西北地质》2007年第2期114-117,共4页Northwestern Geology

基　　金：国家305项目(96-915-05-04)

摘　　要：新疆康古尔塔格金矿发现的副氯铜矿,在我国尚属首次。通过X-衍射分析方法对其做了进一步的确认,通过副氯铜矿的差热分析数据,分析了副氯铜矿的形成条件,由其化学成分计算出晶体化学式。副氯铜矿的发现,进一步丰富了我国氧化带矿物学的内容,而且作为特征矿物,也可做为寻找铜铅锌等多金属硫化物矿床及金铜矿床的找矿标志。The paratacamite has been discovered in Xinjiang Kanggu＇ertage gold mine. It is the first time in China. Analysis-method of X-ray diffraction was used conform the new discovery. The formation condition of paratacamite has analysed by using the dispatch thermal analysis. Crystal formula of paratacamite has been calculated by means of chemical analyses. The discovery of the paratacamite enriches the contents of mineralogy of oxidation zone. The paratacamite, as the characteristic mineral, can be used to find multi-metallic sulfide Cu-Pb-Zn ore deposits and gold-copper deposit.

关 键 词：副氯铜矿 康古尔塔格金矿 氧化带矿物 找矿标志 

分 类 号：P618.51[天文地球—矿床学]