摘要
穷布拉克铜矿产于伊宁铜、铅、锌、铁、铀、钨、锰、煤、白云母成矿带中,属陆相火山热液型铜矿床,成矿作用大致经历了早期火山活动期和中期火山活动期两个成矿期,矿区发现大小不等的数条铜矿体,产于二叠纪火山岩中。在对穷布拉克铜矿床的成矿地质背景及矿区地质特征进行了系统研究的基础上,文章对矿区的矿床成因及找矿标志进行了分析,从而推断该区具有良好的铜矿找矿前景。
The Qiongbulake copper deposit is located in copper, lead, zinc, iron, uranium, tungsten, manganese, coal and muscovite ore belt in Yining county, is a continental volcanic hydrothermal copper deposit, which mineralization has gone through two ore - forming stages from the early volcanic activity to medium - term period of volcanic activity, several copper ore bodies produced in the Permian volcanic rocks are found in this mining area. Based on the study on geological background and mining geology of Qiongbulake copper deposit, the author analyzed the genesis of mining and prospecting criteria , and inferred that the area had good copper ore prospects.
出处
《矿产勘查》
2012年第5期612-617,共6页
Mineral Exploration
关键词
穷布拉克铜矿
火山热液型铜矿
矿床成因
新疆
Qiongbulake copper deposits
volcanic hydrothermal copper mine
genesis
Xinjiang
