| 贵州省从江县高增锰矿矿床地质特征及成因浅析 |
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| 引用本文： | 袁景国,朱德彬.贵州省从江县高增锰矿矿床地质特征及成因浅析[J].华南地质与矿产,2008(3):64-67. |
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| 作者姓名： | 袁景国 朱德彬 |
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| 作者单位： | 1. 贵州省地矿建设工程施工公司,贵阳,550002
2. 贵州省地质矿产勘查开发局106地质大队,贵州,遵义,563000;贵州大学研究生院,贵阳,550003 |
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| 基金项目： | 参加野外调查工作的还有李沛刚、殷科华、陈强、潘忠华等同志,在此表示感谢! |
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| 摘 要： | 从江县高增锰矿严格受控于地层层位和古构造，矿体呈层状、似层状产于南华系大塘坡组底部灰色、浅黑灰色含炭粉砂质粘土岩中，本文总结分析了高增锰矿床矿床地质及矿石质量特征、分析研究成锰期沉积环境，认为该矿床属浅海海湾相沉积型碳酸锰矿床，为黔东及邻区又一典型南华纪“大塘坡式”锰矿床。
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| 关 键 词： | 锰矿 矿床地质特征 成因分析 从江 贵州 |
Geology and Genesis of Gaozeng Manganese Deposit in Congjiang Couty,Guizhou Province |
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| YUAN Jing-guo,ZHU De-bin.Geology and Genesis of Gaozeng Manganese Deposit in Congjiang Couty,Guizhou Province[J].Geology and Mineral Resources of South China,2008(3):64-67. |
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| Authors: | YUAN Jing-guo ZHU De-bin |
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| Institution: | YUAN Jing - guo , ZHU De - bin ( 1. Guizhou Geology and Mineral Construction Engineering Constructing Company, Guiyang, 550002, Guizhou, China 2. No. 106 Geological Brigade, Guizhou Bureau of Geology and Minerals Exploration ＆Development, Zunyi 563000, Guizhou , China 3. Post - graduate Department of Guizhou Universist , Guiyang ,550003, Guizhou , China) |
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| Abstract: | Gaozeng manganese deposit is strictly controlled by strata and paleostructure and occurred as stratiform and quasi - strafiform. The host rocks are gray and light black - gray carbon - bearing silty clay rock in lower of Datangpo Formation, Nanhua System. This paper gave a brief describe on geology of the deposit and component of ores. According to study on sedimentary environment on the forming of manganese deposit, we conclude that the deposit belong to sed~ent carbonate type manganese deposit which formed in shallow - sea facies. It is another typical Nanhua System ＂ Datangpo Type＂ manganese deposit in east Guizhou and adjacent region. |
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| Keywords: | manganese geology genesis Gaozeng manganese deposit Congjiang County Guizhou |
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