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云南大红山铜铁矿床构造控矿规律初探
引用本文:肖斌,;范玉华,;李俊,;杨光树,;戚金栋,;孙明书,;覃龙江,;武贤文,;赵应班.云南大红山铜铁矿床构造控矿规律初探[J].矿产与地质,2014(4):439-442.
作者姓名:肖斌  ;范玉华  ;李俊  ;杨光树  ;戚金栋  ;孙明书  ;覃龙江  ;武贤文  ;赵应班
作者单位:[1]云南省昆明理工大学国土资源工程学院,昆明650092; [2]云南省地质调查院,昆明650216; [3]玉溪大红山矿业有限公司,云南玉溪653405
基金项目:由云南新平大红山铁矿床矿化富集规律及深部找矿预测研究项目资助。
摘    要:大红山铜铁矿床因其构造环境复杂,矿产储量丰富而备受关注。本文通过对大红山铜铁矿床现有不同分段进行构造编录、化学样品采集分析,并结合前人资料,尝试研究断裂构造与铜铁矿床成矿关系。研究发现,在矿区A29―A40勘探线之间深部铁矿体受EW向和NE向断层控制赋存产出。

关 键 词:铜铁矿床  矿床地质特征  构造控矿  大红山  云南

A study on tectonic ore-controlling regularity of Dahongshan Cu-Fe deposit in Yunnan
Institution:XIAO Bin,FAN Yu-hua,LI Jun,YANG Guang-shu,QI Jin-dong,SUN Ming-shu,QIN Long-jiang,WU Xian-wen,ZHAO Ying-ban(1. Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming , Yunnan 650092;2. Yunnan Institute of Geological Survey, Kunming, Yunnan 650216;3. Yuxi Dahongshan Mining Co. , Ltd. , Yuxi, Yunnan 653405)
Abstract:Dahongshan Cu-Fe deposit attracts broad attention because of its complicated tectonic setting and a-bundant mineral reserves.This paper conducts tectonic logging and chemical sample collection and analysis in different sections of Dahongshan Cu-Fe deposit.Based on historical literature,this paper studies the rela-tionship between faulted structure and mineralization of Cu-Fe deposits.The study indicates that the occur-rence of deep lying iron ore-bodies between A29 and A40 prospecting lines are controlled by EW-trending and NE-trending faults.
Keywords:Fe-Cu deposit  geological characteristic of deposit  tectonic ore-controlling  Dahongshan  Yun-nan
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