| 贵州省排庭金矿地质特征与成因分析 |
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| 引用本文： | 伍守荣.贵州省排庭金矿地质特征与成因分析[J].矿产与地质,2008,22(1):55-61. |
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| 作者姓名： | 伍守荣 |
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| 作者单位： | 昆明理工大学国土资源工程学院,云南,昆明,650093;贵州省有色地质勘查局一总队,贵州,清镇,551400 |
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| 基金项目： | 国家资源补偿费矿产资源勘查项目 |
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| 摘 要： | 排庭金矿是贵州三都——丹寨锑、汞、金成矿带上，继苗龙锑-金矿、宏发厂汞-金矿后首次发现的产于中下寒武统独立型的微细浸染型金矿，其矿体受断裂构造、地层、岩性等因素控制，矿床规模为中型。对该矿床的地质特征及成因进行总结和分析，对于华南褶皱带与扬子准地台过渡带寻找寒武纪地层中的微细浸染型金矿具有重要的借鉴和指导意义。
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| 关 键 词： | 金矿 成因分析 地质特征 排庭 贵州 |
| 文章编号： | 1001-5663(2008)01-0055-07 |
| 修稿时间： | 2007年8月20日 |
Geological characteristics of the Paiting Au deposit with its genesis analysis, Guizhou Province |
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| WU Shou-rong.Geological characteristics of the Paiting Au deposit with its genesis analysis, Guizhou Province[J].Mineral Resources and Geology,2008,22(1):55-61. |
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| Authors: | WU Shou-rong |
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| Institution: | WU Shou-rong (1. Faculty of Land Resouce Engineering of Kunming University of Science and Technology, Kunming 650093,China; 2. No. 1 General Geological Team of Guizhou Nonferrous Metals Geo-exploration Bureau, Qingzhen, Guizhou 550005, China) |
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| Abstract: | The Paiting Au deposit is a Mid-Lower Cambrian independent micrograined disseminated gold mine occurred in Sandu-Danzhai metallogenic belt for Sb,Hg, Au deposits, which has been firstly found afer the discovery of Miaolong Sb-Au deposit, Hongfachang Hg-Au deposit. The orebodies of the Pairing Au deposit, which is a middle scale depsoit, are controlled by the factors of fault structure,strata and lithology etc. It has concluded and analyzed the geological characteristics and the genesis of this deposit, which will be a significant reference and guidance for the prospecting of Cambrian micrograined disseminated Au deposit in the transition zone between South China fold belt and Yangtze paraplatform. |
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| Keywords: | Au deposit genesis analysis geological characteristics Paiting Guizhou |
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