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| 平朔露天矿太原组11^#和9^#煤层的沉积环境分析 | |
| 引用本文： | 程东 柴东浩. 平朔露天矿太原组11^#和9^#煤层的沉积环境分析[J]. 高校地质学报, 1998, 4(4): 465-472 |
| 作者姓名： | 程东 柴东浩 |
| 作者单位： | [1]山西大学师范学院地理系 [2]山西省地质科学研究所 |
| 基金项目： | 煤炭工业部I类科研项目 |
| 摘 要： | 平塑露天矿的露采煤层，即１１＾＃和９＾＃煤层是上石炭统太原组Ⅱ－Ⅲ层段扇三角洲－泻湖及扇三角洲－潮坪环境的产物。厚４ｍ的１１＾＃煤层形成于扇三角洲－潮坪环境中，厚１５ｍ的９＾＃煤层形成了扇三角洲平原，扇三角洲前缘（北西部）以及覆水较深的泻湖（中南部）环境中。 |
| 关 键 词： | 露天煤矿 太原组 煤系 沉积环境 煤矿床 |
| 收稿时间： | 1998-12-20 |
| 修稿时间： | 1998-12-20 |
SEDIMENTARY ENVIRONMENT OF 11 # AND 9 # COALS OF TAIYUAN FORMATION AT PINGSUO OPEN PIT MINE |
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| Cheng Dong Shen Fang. SEDIMENTARY ENVIRONMENT OF 11 # AND 9 # COALS OF TAIYUAN FORMATION AT PINGSUO OPEN PIT MINE[J]. Geological Journal of China Universities, 1998, 4(4): 465-472 | |
| Authors: | Cheng Dong Shen Fang |
| Affiliation: | 1. Geographic Department, Shanxi Teach’s College Shanxi University; 2. Shanxi Institute of Geological Sciences, Taiyuan 030012 |
| Abstract: | The 11# and 9# coals, exposed and mined at Pingsuo open-pit mine, occur in Ⅱ-Ⅲ intervals of the Taiyuan Formation, Upper Carboniferous. They were accumulated in environment of fan delta-1agoon and fan delta-tidal flat. The 4m thick 11# coal was formed in an environment of fan delta-tidal flat and the 15m thick 9# coal in all environment of fan deltaic plain, fan delta front and lagoon revering with deep water. |
| Keywords: | Pingsuo open pit mine Taiyuan Formation coal measure sedimentary environment fan delta lagoon. |
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