普鲁裂谷火山岩带块状硫化物矿床特征及找矿远景分析  

CHARACTERISTICS OF THE MASSIVE SULFIDE DEPOSIT IN THE VOLCANIC ROCK ZONE OF THE PULU RIFT AND THE PROSPECTING POTENTIIAL

作　　者：李博秦[1] 

机构地区：[1]中国地质大学资源学院,武汉430074

出　　处：《陕西地质》2002年第2期59-65,共7页Geology of Shaanxi

摘　　要：普鲁裂谷火山岩带是在 1∶2 5万《于田幅》地质调查中首次发现的 ,该带近东西向展布 ,规模巨大。是西昆仑地区块状硫化物矿床形成的重要区段 ,区内已发现硫化物矿床 (点 )数十处 ,典型的矿床 (点 )有阿克塔什铜矿床、塔木其铜、锌矿点、大勒大铜 (金 )矿点、上其汗铜、锌矿床等。其成矿特征类似于塞浦路斯型 。The volcanic rock zone in Pulu Rift, which extents at nearly east to west direction, was first discovered in geological surveying of the Yutian quadrangle scale (1∶250,000) in 2000. It is a significant portion for forming the massive sulfide deposits in the west Kunlun area, in which tens of sulfide deposits (occurrences) have been found, including the Arketashi copper deposit, Tamuqi copper zinc occurrences, Daleda copper (gold) mineralization and Shangqihan copper zinc deposit. Mineralization in this zone has similar features to the Cyprus type and the formation of this zone are found to be closely related to the Pulu volcanic rocks.

关 键 词：裂谷火山岩带 成矿地质特征 找矿远景 地质调查 硫化物矿床 

分 类 号：P618.2[天文地球—矿床学]