摘要
在系统总结土耳其库克罗恩锑矿床成矿地质背景、矿床地质特征、矿床地球化学的基础上,分析了矿床控矿因素,总结了矿床成因。库克罗恩锑矿床矿化富集与地层、地质构造、蚀变等控矿因素密切相关。通过控矿因素分析,结合矿床地质特征,认为库克罗恩锑矿为浅成热液充填型矿床。
On the basis of systematically summarizing ore-forming geological background, ore geological characteristics and ore geo- chemistry of Turkey Kukeluoen antimony deposit, the paper ana- lyzed the ore-controlling factors, summariged ore genesis. The mineralization enrichment of Kukeluoen antimony deposit is closely related with its stratigraphy, geologic structure, altera- tion and other ore-control factors. Through analysis of ore-con- trolling factors, combined with the geological characteristics, the paper considers Kukeluoen antimony deposit shouid be a type of epithermal filled deposits.
出处
《西部探矿工程》
CAS
2012年第9期104-106,共3页
West-China Exploration Engineering
关键词
土耳其
锑矿床
地质特征
矿床成因
Turkey
antimony deposit
geological characteris- tics
ore genesis