哈萨克斯坦斑岩铜矿地质-成因模式  

THE GEOLOGY-GENETIC MODEL OF KAZAKHSTAN PORPHYRY COPPER DEPOSIT

作　　者：宋志齐 高鹏 祁世军 成守德 

机构地区：[1]新疆维吾尔自治区地质矿产研究所,新疆乌鲁木齐830000

出　　处：《新疆地质》2009年第B12期70-75,共6页Xinjiang Geology

基　　金：中国大陆周边地区主要成矿带成矿规律对比及潜力评价计划项目--中哈合作巴尔喀什-准噶尔斑岩铜矿成矿条件对比研究(1212010661315);中亚五国矿产资源勘查开发指南(1212010811066);国家科技部"十一五"科技支撑项目-兴都库什-西昆仑成矿带岩浆成矿作用对比研究(2006BAB01A03-2-2)共同资助

摘　　要：简述了哈萨克斯坦斑岩铜矿的成矿特征并划分出3种类型,分别为次生石英岩化-泥化斑岩铜矿——科翁腊德(коунрадский)型;黄铁细晶岩化-粘土化斑岩铜矿——阿尔马林(алмалинсий)型;青磐岩化细脉浸染型斑岩铜矿——博萨库里(бозшакльский)型.其中,科翁腊德型最靠近地表,阿尔马林型居中,博萨库里型最深.对各类型铜矿的基本特征进行了概述.The character of metallogenic of kazakhstan porphyry copper deposits are brief described in this article, and they are divided into three types, respectively the type of Konyrat-secondary quartzite-argillization porphyry copper deposit, the type of Almaly-beresitization-clayization porphyry copper deposit, the type of Bozshakol-propylitization netted-disseminated porphyry copper deposit, type of Konyrat is very near to surface, Almaly is in the middle, and type of Bozshakol is the deepest. The character of metallogenic of different types are summarized.

关 键 词：哈萨克斯坦 斑岩铜矿 成矿特征 热液蚀变 

分 类 号：P618.41[天文地球—矿床学]