| 福建泰宁李家坊金矿地质特征与成因分析 |
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| 引用本文： | 周延召,黄新鹏.福建泰宁李家坊金矿地质特征与成因分析[J].福建地质,2011,30(2):108-112. |
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| 作者姓名： | 周延召 黄新鹏 |
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| 作者单位： | 福建省地质调查研究院,福州,350013 |
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| 摘 要： | 泰宁李家坊金矿位于崇安-石城深断裂带中段,矿体是在区域变质、构造活动、岩浆侵入的长期作用下形成的,矿体主要贮存于中元古代交溪组混合岩化变质岩中,为断裂破碎带蚀变岩型金矿,主要成矿期为志留纪.
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| 关 键 词： | 金矿 地质特征 成因分析 李家坊 |
Geological Features and Cause Analysis of the Lijiafnag Gold Deposit in Taining County, Fujian Province |
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| Zhou Yanzhao,Huang Xinpeng.Geological Features and Cause Analysis of the Lijiafnag Gold Deposit in Taining County, Fujian Province[J].Geology of Fujian,2011,30(2):108-112. |
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| Authors: | Zhou Yanzhao Huang Xinpeng |
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| Institution: | (Fujian Institute of Geology Survey and Research,Fuzhou,350013) |
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| Abstract: | The Lijiafang gold deposit located at the middle of Chongan-Shicheng deep fracture zone.The ore body formed under the long-term effects of regional metamorphism、tectonic movement and magma intrusion,and mostly hosted in migmatization metamorphic rock of Mesoproterozoic Jiaoxi group.The deposit is faulted and shattered zone-altered rock type gold deposit,and mostly formed in Silurian period. |
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| Keywords: | gold deposit geological features cause analysis Lijiafang |
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