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作 者:韩红卫[1] 周忠宇[2] 欧阳国湘[1] 石良[3] 马慧[3]
机构地区:[1]新疆维吾尔自治区地质矿产勘查开发局第三地质大队,新疆库尔勒841000 [2]新疆巴音郭楞蒙古自治州国土资源局,新疆库尔勒841000 [3]新疆维吾尔自治区地质矿产勘查开发局第七地质大队,新疆乌苏833000
出 处:《新疆地质》2006年第3期256-260,共5页Xinjiang Geology
基 金:新疆维吾尔自治区矿产资源补偿费项目(2004034)资助
摘 要:卡特里西铜锌矿是近年在新疆南部昆仑山一带发现的、规模最大的有色金属矿床.矿床产于下石炭统托库孜达坂群火山岩地层中,矿体分布明显受地层控制.含矿岩性为双峰式火山岩建造上部的灰绿色基性凝灰岩,矿体多呈平行层状、似层状、透镜状分布于灰岩中及灰岩与含碳粉砂岩的接触处.该矿为海相火山岩型铜矿.主成矿元素为铜、锌,伴生元素为银、铅、硫,共有14个矿体,其中Ⅵ、Ⅷ号矿体为主矿体,矿石品位较富,目前估算铜、锌资源量均超过中型.通过进一步的地质、地球化学、地球物理工作表明,矿床主矿体向深部仍有较大延深,预测该矿床规模有望达到大型.Katelixi Cu-Zn deposit is currently the considerable nonferrous metal deposit in the Kunlun Mountain area of Xinjiang, the volcanic strata of Tuokuzidaban group in Carboniferous controlled ore bodies. The mineralization rock is gray-green tuff and intercalated in limestone and silt rock as layer and lens. this deposit is a copper deposit of marine facies's volcano rock type. Copper is the main metallogenetic element, zinc is the associated element, it is silver ,lead and sulphur that companion living in it. there are 14 ore bodies totally, the Ⅵ and Ⅷ number ore body in which are main ore bodys ,the ore grade is high. Currently, we estimated that the scale of copper and zinc would be above medium-sized. We detect the depths of the main ore body through geology and geophysical exploration, and draw a same conclusion, that, the deposit has a further extention to the depths, and maybe it's scale can reach large-sized, and it's periphery also has fairly good prospect of looking for mineral deposits.
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