| 万山特区铁门闩碳酸锰矿床特征及成因浅析 |
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| 引用本文： | 舒多友. 万山特区铁门闩碳酸锰矿床特征及成因浅析[J]. 贵州地质, 2000, 17(4): 269-272 |
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| 作者姓名： | 舒多友 |
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| 作者单位： | 贵州省地勘局一○三地质队贵州铜仁 554300 |
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| 摘 要： | 铁门闩碳酸锰矿受控于地层层位，呈层状，似层状、透镜状沿震旦系下统大塘坡组一段（Ｚ１ｄ）富含有机质炭质页岩下部顺层产出。根据含锰岩系特征，矿体形态规模，矿石质量的分析研究，该锰矿床应属浅海沉积型碳酸锰矿。
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| 关 键 词： | 矿床成因 碳酸锰矿床 地质特征 含锰岩系特征 |
| 文章编号： | 1000-5943(2000)04-0269-04 |
| 修稿时间： | 1999-11-18 |
Primary Analysis on Feature and Genesis of Tiemenshuan Carbonate Manganese Deposit in Wangshan of Guizhou |
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| SHU Duo_you. Primary Analysis on Feature and Genesis of Tiemenshuan Carbonate Manganese Deposit in Wangshan of Guizhou[J]. Guizhou Geology, 2000, 17(4): 269-272 |
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| Authors: | SHU Duo_you |
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| Abstract: | Tiemenshuan manganese carbonate deposit is controlled by stratum horizon, which normally occurs in layers and similar layers and lentiform along a block of lower organic carbonate_rich shale of Datangpo formation of upper Sinian system. Through dealing with feature of manganese_bearing rocks, scale and shape of ore and ore quantity, this manganese deposit should be classified to carbonate manganese deposit of shallow_marine sedimentary. |
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| Keywords: | carbonate manganese genesis of deposit Tiemenshuan Wanshan |
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