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山西东腰庄绿岩带型金矿床地质特征及找矿标志
引用本文:董培培,刘德武,刘玉翠,王金芳,白卉,杨轩.山西东腰庄绿岩带型金矿床地质特征及找矿标志[J].黄金科学技术,2011,19(4):42-44.
作者姓名:董培培  刘德武  刘玉翠  王金芳  白卉  杨轩
作者单位:石家庄经济学院资源学院,河北 石家庄 050031
摘    要:东腰庄绿岩带型金矿床赋存于五台山绿岩带之中,赋矿地层为新太古界五台群鸿门岩组绿片岩,具有明显的层控性。该矿床由Ⅰ、Ⅱ、Ⅲ号 3 个矿体构成,矿体呈似层状和脉状,走向 NE。容矿岩石为强烈黄铁矿化、硅化和碳酸盐化的绢云钠长片岩、绢云石英片岩、绢云钠长绿泥片岩和变辉绿岩脉。围岩蚀变发育,主要为硅化、绢云母化、绿泥石化、碳酸盐化和黄铁矿化,由内向外呈现出分带性。矿床具有明显的地质、地球物理及地球化学找矿标志。

关 键 词:金矿床  绿岩带  找矿标志  东腰庄  山西省  
收稿时间:2011-05-13
修稿时间:2011-07-19

The Geological Characteristics and Prospecting Criteria of Dongyaozhuang Greenstone Belt Gold Deposit,Shanxi Province
DONG Peipei,LIU Dewu,LIU Yucui,WANG Jinfang,BAI Hui,YANG Xuan.The Geological Characteristics and Prospecting Criteria of Dongyaozhuang Greenstone Belt Gold Deposit,Shanxi Province[J].Gold Science and Technololgy,2011,19(4):42-44.
Authors:DONG Peipei  LIU Dewu  LIU Yucui  WANG Jinfang  BAI Hui  YANG Xuan
Affiliation:College of Resources,Shijiazhuang University of Economics,Shijiazhuang 050031,Hebei,China
Abstract:Dongyaozhuang greenstone belt gold deposit occur in the greenstone belt of Wutai mountain,the ore iormation is new Archean Wutai group Hongmen rock group green schist,it has obvious layer controlling.The deposit is formed by three orebodies, Ⅰ , Ⅱ, Ⅲ ,the shape of orebody is bedded and vein,north-east trending.The bearing-rock is albite sericite schists,quartz schist, chlorite albite and diabase dikes,which are strongly pyritization,silicification and carbonate.The wall-rock alteration develop,the alteration is mainly quzatz,sericite,ehlorite carbonate and pyrite,from inside to outside,it shows zonation.The deposit has obvious geological,geophysical and geochemical prospecting criteria.
Keywords:Gold deposit  Greenstone belt  Prospecting criteria  Dongyaozhuang  Shanxi Province  
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