| 北宿井田高岭岩矿床特征研究 |
| |
| 引用本文： | 苏淑荣,牛磊,曹广宇.北宿井田高岭岩矿床特征研究[J].山东科技大学学报(自然科学版),2000,19(3):55-58. |
| |
| 作者姓名： | 苏淑荣 牛磊 曹广宇 |
| |
| 作者单位： | 山东兖矿集团地质工程公司山东邹城 273500 |
| |
| 摘 要： | 对北宿井田内煤１８底板高岭岩矿床的赋存状态、岩性特征、矿物成分及化学组成进行了详细研究，并探讨了高岭岩的沉积环境及沉积规律。研究表明北宿井田高岭岩矿床分布稳定，质量较好，质量较好，具有重要的开采价值；其形成环境与成煤环境相近似，系泻湖、泥坪等弱水动力环境中由粘土质点及细粒陆源碎屑沉积而成，其母岩为酸性岩为酸性岩浆岩。
|
| 关 键 词： | 高岭岩 矿床特征 沉积环境 北宿井田 赋存状态 |
| 文章编号： | 1000-2308(2000)03-0055-04 |
| 修稿时间： | 2000年1月20日 |
Analysis on Sedimentary Characteristics of the Kaolinite Deposite in Beixu Coal Mine |
| |
| SU Shu rong,NIU Lie,CAO Guang yu.Analysis on Sedimentary Characteristics of the Kaolinite Deposite in Beixu Coal Mine[J].Journal of Shandong Univ of Sci and Technol: Nat Sci,2000,19(3):55-58. |
| |
| Authors: | SU Shu rong NIU Lie CAO Guang yu |
| |
| Abstract: | This paper gives a detailed study on the depositing state ,lithology and mineralogy,etc.of the kaolinite in the floor of the No.18 coal seam in Beixu Coal Mine,and probes into the sedimentary environment and distribution law of the mineral layer,Study shows that the kaolinite in the Beixu Coal Mine distributed stably with good quality and formed in the similar environment with coal seam.They originated from the fine grained clastic sediments which were deposited in the weak hydrologic environment such as lagoon and mud flat. |
| |
| Keywords: | kaolinite deposite characteristics sedimentary environment Beixu Coal Mine |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
