| 平邑县铜石次火山杂岩体区金矿化类型及其成矿地质特征 |
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| 引用本文： | 祝德平,张晓梅,李守全,齐可昆. 平邑县铜石次火山杂岩体区金矿化类型及其成矿地质特征[J]. 黄金, 2000, 0(8) |
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| 作者姓名： | 祝德平 张晓梅 李守全 齐可昆 |
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| 作者单位： | 山东省平邑黄金有限责任公司 |
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| 摘 要： | 平邑县铜石次火山杂岩体区是鲁西黄金发展新区 ,众多的金矿化体聚于杂岩体的内部及周边 ,构成了多种定位样式矿化群聚的组合体。本文归纳了该区金矿化类型 ,并对成矿地质特征、矿床成因及金的富集规律作了分析。
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| 关 键 词： | 次火山杂岩体 金矿化类型 地质特征 矿床成因 富集规律 铜石 |
The mineralization types of Tongshi district of secondary volcanic complex rock mass in Pingyi County and their geological feature of mineralization |
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| Zhu Deping et al.. The mineralization types of Tongshi district of secondary volcanic complex rock mass in Pingyi County and their geological feature of mineralization[J]. Gold, 2000, 0(8) |
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| Authors: | Zhu Deping et al. |
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| Affiliation: | Pingyi Gold Ltd.Co.of Shandong Province |
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| Abstract: | Tongshi district of secondary volcanic complex rock mass is a new district of gold development in the west part of shandong Province.Much more gold mineralized mass assemble in the interior and periphery of complex rock mass to form multi type located pattern of mineralization groups.In this paper,the gold mineralization types in this district are summed up and the geological feature of mineralization,the genesis of gold deposit and the regularity of gold concentration are analyzed. |
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| Keywords: | secondary volcanic complex rock mass gold mineralization type geological feature genesis of deposit regularity of concentration Tongshi |
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