| 大方五凤井田6含煤段沉积环境及6中薄煤带成因分析 |
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| 引用本文： | 曹志德,熊孟辉.大方五凤井田6含煤段沉积环境及6中薄煤带成因分析[J].贵州地质,2008,25(4). |
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| 作者姓名： | 曹志德 熊孟辉 |
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| 作者单位： | 1. 贵州省煤田地质局地质勘察处,贵州,贵阳,550006
2. 贵州省煤田地质局地质勘察研究院,贵州,安顺,561000 |
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| 摘 要： | 利用地质报告资料分析了五凤井田6含煤段沉积环境,探讨了首采区内6中煤薄煤带成因,认为6中煤薄煤带是由于砂体的冲刷作用形成的。
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| 关 键 词： | 五凤井田 6含煤段 沉积环境 薄煤带 成因分析 |
Analyses on the NO.6 Coal-bearing Sedimentary Environment and NO.6 Middle Thin-coal Area Causation of Wufengjing Orefield in Dafang |
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| CAO Zhi-de,XIONG Meng-hui.Analyses on the NO.6 Coal-bearing Sedimentary Environment and NO.6 Middle Thin-coal Area Causation of Wufengjing Orefield in Dafang[J].Guizhou Geology,2008,25(4). |
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| Authors: | CAO Zhi-de XIONG Meng-hui |
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| Abstract: | With the geological information,the sedimentary environment of NO.6 coal-bearing section was analyzed and the causation of the NO.6 thin-coal area were discussed.It's thought that the NO.6 thin-coal area was caused by flush effect of sand body. |
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| Keywords: | Wufeng orefield NO 6 coal-bearing section sedimentary environment thin-coal area causation analyses |
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