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米仓山地区金矿特征及找矿远景分析
引用本文:陈友良,王淦顺,魏继生,李文贤.米仓山地区金矿特征及找矿远景分析[J].四川地质学报,2010,30(3):288-290.
作者姓名:陈友良  王淦顺  魏继生  李文贤
作者单位:1. 成都理工大学,成都,610059
2. 核工业280研究所,四川,广汉,618300
摘    要:米仓山地区的金矿主要产在太古代—早元古代后河岩群绿岩和澄江期陆壳重熔S型花岗岩中,金矿化主要受SN、NE向的韧脆性剪切带所控制,发育多期次、多阶段的热液蚀变活动,成矿物质主要来源于澄江期重熔花岗岩浆期后含金热液,还包括部分变质热液。米仓山地区金矿的找矿前景广阔。

关 键 词:,金矿,韧脆性剪切带,找矿远景,米仓山

Geological Features and Prospecting Potential for Au Deposits in the Micang Mountains
Chen Youliang,WANG Ganshun,WEI Jisheng,LI Wenxian.Geological Features and Prospecting Potential for Au Deposits in the Micang Mountains[J].Acta Geologica Sichuan,2010,30(3):288-290.
Authors:Chen Youliang  WANG Ganshun  WEI Jisheng  LI Wenxian
Institution:1-Chengdu University of Technology,Chengdu 610059;2-Institute No.280,CNNC,Guanghan,Sichuan 618300)
Abstract:Au deposits in the Micang Mountains are confined to greenstone of the Archean-Lower Proterozoic Houhe Group and to S-type granite in Chengjiang period.It was controlled by longitudinal and NE-trending brittle-ductile shear zones.The ore material was derived mostly from postmagmatic Au-bearing fluids of the Chengjiang anatectic granite.
Keywords:gold deposit  brittle-ductile shear zones  prospecting perspective  Micang Mountains
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