| 安徽省五河县荣渡金矿床地质特征及成因 |
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| 引用本文： | 李建设,吴礼彬.安徽省五河县荣渡金矿床地质特征及成因[J].安徽地质,2001,11(1):38-43. |
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| 作者姓名： | 李建设 吴礼彬 |
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| 作者单位： | 1. 安徽省地矿局312地质队,安徽,蚌埠,233040
2. 安徽省地矿局312地质队,安徽,蚌埠,233040;安徽省地质调查院,安徽,合肥,230001 |
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| 基金项目： | 安徽省五河荣渡金矿成矿条件及成矿预测项目;; |
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| 摘 要： | 五河荣渡金矿床是多种成矿作用叠加、改造的产物，为燕山期中高温岩浆热液形成的。成矿物质主要来自岩浆期后热液，其次与围岩、脉岩等关系密切。郯庐韧一脆性剪切带是主要的导矿构造。其次级断裂是主要容矿场所。
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| 关 键 词： | 金矿床地质特征 矿床成因 蚌埠隆起区 |
| 文章编号： | 1005-6157(2001)01-0038-06 |
| 修稿时间： | 1999年9月23日 |
GEOLOGICAL FEATURES AND ORIGIN OF THE RONGDU GOLD DEPOSIT, WUHE, ANHUI PROVINCE |
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| LI Jian-she,WU Li-bin.GEOLOGICAL FEATURES AND ORIGIN OF THE RONGDU GOLD DEPOSIT, WUHE, ANHUI PROVINCE[J].Geology of Anhui,2001,11(1):38-43. |
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| Authors: | LI Jian-she WU Li-bin |
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| Abstract: | The Rongdu gold deposit is formed by the Yenshanian mid - high temperature magmatic hydrothermalism as a product of superimposition and reworking by many ore - forming processes. The metallogenetic substance is derived mainly from postmagmatic hydrothermal solution, secondarily bound up with wallrock and dike rock. The Tanlu ductile brittle shear zone is the major structure as passageway for ore fluid and its secondary faults are the main host. |
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| Keywords: | geological features of gold deposit origin of deposit Bengbu uplifting area |
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