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| 青城子矿田金凤金银多金属矿床地质特征及成因探讨 | |
| 引用本文： | 刘恒刚,陈贺,周传勤,郑廷,李太阳.青城子矿田金凤金银多金属矿床地质特征及成因探讨[J].黄金,2009,30(4):17-21. |
| 作者姓名： | 刘恒刚 陈贺 周传勤 郑廷 李太阳 |
| 作者单位： | 1. 辽宁省凤城市黄金管理局 2. 凤城市白云金矿 3. 辽宁有色地质局103队 |
| 摘 要： | 阐述了青城子矿田金凤金银多金属矿床成矿地质背景及矿床地质特征,并对成矿机制进行了研究和分析,指出了火山喷流沉积变质地层是成矿基础,韧-脆性剪切构造是控矿条件,岩浆热液提供了成矿物质及热动力,是成矿关键。因此,金凤金银多金属矿床属火山喷流沉积—岩浆热液叠加型矿床。 |
| 关 键 词： | 金凤金银多金属矿床 韧-脆性剪切构造 火山喷流作用 岩浆热液 |
Geological characteristics and genesis of Jinfeng gold-silver polymetallic deposit in Qingchengzi ore field |
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| Liu Henggang,Chen He,Zhou Chuanqin,Zheng Ting,Li Taiyang.Geological characteristics and genesis of Jinfeng gold-silver polymetallic deposit in Qingchengzi ore field[J].Gold,2009,30(4):17-21. | |
| Authors: | Liu Henggang Chen He Zhou Chuanqin Zheng Ting Li Taiyang |
| Affiliation: | 1.Fengcheng Bureau of Gold Industry Administration;Liaoning Province;2.Fengcheng Baiyun Gold Mine;3.103 Team;Bureau of Non-ferrous Geology of Liaoning Province |
| Abstract: | The paper introduced the geological mineralization background and geological characteristics of Jinfeng gold-silver polymetallic deposit in Qingchengzi ore field.Researches on mineralization mechanism were carried out too.It was put forward that the volcanic eruption sedimentary metamorphic strata were the mineraliztion foundation;the ductile-brittle shear structure was the ore-controlling condition;the magmatic hydrothermal fluid supplied mineralization substance and thermal power.The deposit was a compoun... |
| Keywords: | Jinfeng gold-silver polymetallic deposit ductile-brittle shear structure volcanic eruption fluid magmatic hydrothermal fluid |
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