摘要
苏吾鲁克铜矿位于昆盖山北坡石炭纪铜、金成矿亚带内(Ⅵ2),该矿带内目前发现的铜矿床点13处,主要产于下石炭统乌鲁阿特组和克孜里奇曼组火山岩中。苏吾鲁克铜矿赋存于下石炭统乌鲁阿特组(C1w)中基性火山岩中,属火山喷发、喷气沉积铜矿床。通过2009年地质找矿工作,共圈出了8条矿体,规模较大的矿体主要有3条。文章通过对矿体特征,矿石物质组分、结构,围岩蚀变,矿质来源分析,探讨了苏吾鲁克铜矿矿床成因并建立了该矿床的成矿模式。
Suwuluke copper ore deposit is located at Cu -Au sub -metallogenic belt （Ⅵ2） of carboniferous system of the north of the Kungai mountain, where 13 copper mineral occurrences have been discovered. Most of them are hosted in Wuluat Group and Kzirichiman Group~ volcanic rock of lower carboniferous series. Suwuluke VMS- type copper ore deposit, is hosted in Wuluat Group （Clw） intermediate -basic volcanic rock. Total 8 ore bodies, including 3 main orebodies were discovered. In this paper, authors discussed the genesis of mineral deposit and metallogenic model of Suwuluke copper ore deposit on the basis of characteristics of orebodies, composition of ore, ore structure, alteration, source of ore - forming materials.
出处
《矿产勘查》
2011年第2期120-125,共6页
Mineral Exploration
关键词
苏吾鲁克铜矿床矿床成因
成矿模式
新疆
Suwuluke copper ore deposit
genesis of ore deposit
metallogenic model
Xinjiang
