| 辽宁凤城荒甸子金矿床地质特征及成因探讨 |
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| 引用本文： | 刘开慧,刘福兴,苏建飞,吴亚顺,杨云鹏.辽宁凤城荒甸子金矿床地质特征及成因探讨[J].吉林地质,2012,31(1):35-40. |
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| 作者姓名： | 刘开慧 刘福兴 苏建飞 吴亚顺 杨云鹏 |
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| 作者单位： | 辽宁省有色地质局一0三队,辽宁丹东,118008 |
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| 摘 要： | 荒甸子金矿床位于辽东金矿化集中区青城子矿田北东部,矿体严格受地层和构造双重控制,并与印支—燕山期岩浆侵入体相关密切。文章通过对荒甸子金矿床成矿地质背景和主矿体60号金脉带地质特征的阐述,说明金矿体与地层、构造、岩浆岩三位一体的关系,为下一步的找矿工作指明方向。
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| 关 键 词： | 荒甸子金矿 60号金脉带 硅化破碎蚀变岩 矿床成因 |
Geological features and genesis of Huangdianzi gold deposit in Fengcheng City,Liaoning Province |
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| LIU Kai-hui,LIU Fu-xing,SU Jian-fei,WU Ya-shun,YANG Yun-peng.Geological features and genesis of Huangdianzi gold deposit in Fengcheng City,Liaoning Province[J].Jilin Geology,2012,31(1):35-40. |
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| Authors: | LIU Kai-hui LIU Fu-xing SU Jian-fei WU Ya-shun YANG Yun-peng |
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| Institution: | 103 Team,Bureau of Nonferrous Metals Geology of Liaoning Province,Dandong 118008,Liaoning,China; |
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| Abstract: | The Huangdianzi gold deposit is located in the Northeastern part of Qingchengzi orefield,concentrated area of the Liaodong gold mine.The ore body is strictly controlled by the strata and structure,and related with Indo-Yanshanian magmatic intrusive closely.Through the metallogenetic geology setting and the geological features of the main ore body No.60 gold veins,this paper explained the relationship between gold ore body and strata,structure and magmatic rocks,show the direction for the future prospecting work. |
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| Keywords: | Huangdianzi gold deposit No 60 gold veins silicide broken altered rocks genesis of deposit |
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