| 湖南水口山铅-锌多金属矿田硅化角砾岩体(带)地质特征与成矿关系 |
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| 引用本文： | 刘省三.湖南水口山铅-锌多金属矿田硅化角砾岩体(带)地质特征与成矿关系[J].矿产与地质,2007,21(2):186-191. |
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| 作者姓名： | 刘省三 |
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| 作者单位： | 湖南省有色地勘局二一七队,湖南,衡阳,421001 |
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| 摘 要： | 水口山铅-锌多金属矿田内的硅化角砾岩体（带）的展布明显地与矿田构造关系密切。根据硅化角砾岩体（带）所处位置的地质环境、构造特征及硅化角砾岩体的产状、成份、胶结物特征的分析,参考镜下鉴定和部分测试资料,将矿田内的硅化角砾岩体（带）分为层间破碎带型、断层破碎型和溢流硅帽泉华型三类,并论述各类硅化角砾岩体与铅锌多金属矿成矿关系的密切程度。
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| 关 键 词： | 铅锌多金属矿田 硅化角砾岩 分类 成矿关系 水口山 湖南 |
| 文章编号： | 1001-5663（2007）02-0186-06 |
| 收稿时间： | 2006-12-10 |
| 修稿时间： | 2006-12-10 |
Geological characteristics of silicified Breccia in Shuikoushan lead zinc polymetallic ore field of Hunan and its association with mineralization |
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| LIU Shen-san.Geological characteristics of silicified Breccia in Shuikoushan lead zinc polymetallic ore field of Hunan and its association with mineralization[J].Mineral Resources and Geology,2007,21(2):186-191. |
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| Authors: | LIU Shen-san |
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| Institution: | No. 217 Team of Hunan Nonferrous Metals Geo-exploration Bureau, Hengyang, Hunan 421001,China |
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| Abstract: | The distribution of silicified breccia(zone) in Shuikoushan lead zinc polymetallic ore field obviously shows close association with ore field structure.The silicified breccia rocks(zones) in the ore field have been classified into three kinds,namely interlayer type,fracture type and sedimentary transformation type,according to the geological environment and structure character of the location where the silicified breccia rocks occur as well as the analysis on the occurrence,composition,cement characteristics of the silicified rocks,with the reference to microscopic identification and some test data.The affinity of various silicified breccia with lead zinc polymetallic deposit was also mentioned in the paper. |
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| Keywords: | lead and zinc polymetallic ore field silicified breccia classification metallogenic association Shuikoushan Hunan |
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