阿舍勒黄铁矿型铜矿床地质特征  

GEOLOGIC CHARACTERISTICS OF THE PYRITE-TYPE COPPER DEPOSIT IN ASHELE

作　　者：赵云长 陈文鳌 候新建 曾桂华 

机构地区：[1]新疆维吾尔自治区地质矿产局第四地质大队

出　　处：《新疆地质》1992年第1期62-73,共12页Xinjiang Geology

摘　　要：本文通过对矿床的成矿地质条件、控矿因素和物质组份的分析研究,认为该矿为火山成因块状黄铁矿型铜矿。矿体受火山机构控制,产于火山穹窿叠加背斜构造中或火山管道及火山口附近。矿体形态复杂、矿床规模大、品位富、矿种多,矿化垂直分带明显,可作为典型矿床进行研究,以期找到同类矿床。Based on the analyses of the ore-forming conditions, ore-controlling factors and compositions , the deposit is regarded as a massive pyrite-type copper deposit of volcanic origin. Controlled by volcanic mechanism, the ore body occurs in the anticlinal structures formed by overlapping dome volcanoes, or volcanic pipes as well as volcanic craters nearby. The deposit is of large scale, high grade and many variety, with a complicated ore body morphology and a clear vertical mineralization belt, so it can be regarded as a typical deposit for searching the others of the same type.

关 键 词：黄铁矿型铜矿 火山机构 阿舍勒 

分 类 号：P5[天文地球—地质学]