兴都库什-西昆仑区域成矿特征  

Regional Metallogenic Characteristics of Hindu Kush-the Western Kunlun

作　　者：祁世军 

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》2013年第4期313-317,共5页Xinjiang Geology

基　　金：中国大陆周边重要成矿带成矿地质条件对比与资源潜力评价;中国与哈萨克斯坦接壤地区成矿规律与找矿远景研究项目(1212011220913)共同资助

摘　　要：兴都库什-西昆仑西构造结为亚洲大陆重要造山带,在漫长的地质历史演化过程中,形成了丰富的矿产资源。从老到新,不同构造阶段,西昆仑、帕米尔、兴都库什等所表现出的矿床类型、成矿系列、成因类型、成矿时代等各具特色,成为全球3大巨型成矿域之——古亚洲洋和特提斯两大成矿域的重要组成部分,也是未来极具找矿潜力的远景区。Hindu Kush-the Western Kunlun tectonic knot is an important orogenic belt of the Asian continent,and formed a rich mineral resources after a long process of geologic evolution history.lt has its own characteristics in deposit types,metallogenic series,genetic type and mineralogenetic epoch manifested by the western Kunlun,Pamir and Hindu Kush from different tectonic stages,they are an important part of Paleoasian ocean metallogenic domain and the Tethyan metallogenic domain,and also a potential area for mineral prospecting in the future.

关 键 词：兴都库什 西昆仑 成矿带 成矿时代 

分 类 号：P617[天文地球—矿床学]