首页 | 本学科首页   官方微博 | 高级检索  
     检索      

新疆且末县迪木那里克铁矿床地质特征与找矿潜力分析
引用本文:石福品,陈登辉,张海军.新疆且末县迪木那里克铁矿床地质特征与找矿潜力分析[J].西北地质,2010,43(4):203-208.
作者姓名:石福品  陈登辉  张海军
作者单位:[1]新疆地矿局第三地质大队,新疆库尔勒841000 [2]中国地质调查局西安地质调查中心,陕西西安710054
基金项目:新疆自治区地质勘查基金
摘    要:新疆且末县迪木那里克铁矿床位于阿尔金山南缘大断裂东南侧。通过大量的野外地质工作和室内分析,发现矿体严格受地层控制,产于长沙沟构造蛇绿混杂岩带之中,赋矿岩石以千枚岩为主,属于沉积变质型磁铁矿矿床。初步确定矿区存在一个大的向斜构造,已对主矿体(F e36、F e37)进行了工程控制,新增资源量3 003万t。矿体向深部和外围的延伸情况还未完全控制,而且矿区外围存在大量航磁异常有待进一步查证。说明该矿找矿潜力巨大。

关 键 词:迪木那里克  铁矿床  控矿因素  找矿潜力

Exploration Progress Around Dimnalic Iron Deposit in Qiemo County, Xinjiang
SHI Fu-pin,CHENG Deng-hui,ZHANG Hai-jun.Exploration Progress Around Dimnalic Iron Deposit in Qiemo County, Xinjiang[J].Northwestern Geology,2010,43(4):203-208.
Authors:SHI Fu-pin  CHENG Deng-hui  ZHANG Hai-jun
Institution:1.No.3 Geological Team,Xinjiang Bureau of Geology and Mineral Resources,Korla 841000,China;2.Xi'an Center of Geological Survey,CGS,Xi'an 710054,China)
Abstract:The geological exploration project from Xinjiang geological exploration found preliminarily set up that there might exist a large synclinal structure and the amount of mineral resources has been increased;a new surface magnetic anomaly has been delineated around the area and there occurs limestone,phyllite,and pyrite-bearing phyllite which is characterized as the roof of Dimunalike iron deposit,with nearly horizontal occurrence,where it might exist magnetite-bearing beds and might have prospects for iron ore resources.
Keywords:Dimunalike  Iron ore deposit  ore-control factor  prospects
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号