摘要
川乌鲁地区金铜多金属矿矿体主要赋存于泥盆—石炭系科克莫依纳克岩体内外接触带,受岩体或构造裂隙控制,区域内成矿地质条件优越.在综合分析矿区资料基础上,归纳矿床地质特征,探讨矿床成因,提出下一步找矿方向,为在西南天山寻找类似矿床提出工作思路.
Chuanwulu areas of gold-copper-polymetallic mine on the main occurrence Devonian - Tenneco Carboniferous Kokomo according to contacts inside and outside rock band, or by tectonic rock fissures control, regional geological favorable conditions, comprehensive analysis of the mining area on the basis of information, summarized deposit geology, explore genesis proposed the next step prospecting direction, and the Tianshan Mountains in the southwest to find a similar deposit ideas for work.
出处
《新疆地质》
CAS
CSCD
北大核心
2009年第1期28-31,共4页
Xinjiang Geology
基金
新疆阿合奇县托什干河上游一带1:5万区调招标项目(XJQDW2003-17)
新疆地矿局基数地质勘查项目(XGMB200602)共同资助
关键词
川乌鲁地区
金铜多金属矿
地质特征
矿床类型
找矿方向
Chuanwulu region
Gold-copper-polymetatlic ores
Geological features
Deposit type
Prospecting direction
