| 陆振裕,尹灵强,施翔,王忠华.江苏仑山金矿地质特征与矿床成因探讨[J].矿产勘查,2018,9(5):858-864 |
| 江苏仑山金矿地质特征与矿床成因探讨 |
| Research on geological characteristics and ore deposit genesis of Lunshan gold deposit, Jiangsu |
| 投稿时间：2018-03-23 |
| DOI： |
| 中文关键词: 江苏镇江 仑山金矿 地质特征 矿床成因 浅成低温热液 |
| 英文关键词: Zhenjiang, Jiangsu, Lanshan gold deposit, geological characteristics, genesis of deposit, low temperature hydrothermal |
| 基金项目:江苏省地质矿产局科研项目(编号:2014-KY-5)资助。 |
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| 中文摘要: |
| 仑山金矿位于江苏省镇江市西南,为一小型金矿床,金矿体赋存于白垩系杨冲组中,容矿岩石为碳质泥岩和泥质粉砂岩。文章从金矿的区域地质、矿区概况、矿体特征、金的赋存状态等方面入手,分析了金矿的地质特征,探讨了矿床的成因机理,认为仑山金矿应为浅成低温热液型矿床。 |
| 英文摘要: |
| The Lunshan gold deposit is located in the southwest of Zhenjiang, Jiangsu province. It is a small gold deposit, and the gold ore body is deposited in the cretaceous Yangchong formation, and the rock is carbonaceous mudstone and argillaceous siltstone. This paper describes the present situation of regional geology, mining area, ore body characteristics, gold occurrence state, and other aspects. Then analyze the ore-forming geological characteristics, and discuss the genetic mechanism of ore deposit, finally draw the conclusion:The mineralization mechanism of Lunshan gold deposit should be a shallow low-temperature hydrothermal gold deposit. |
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