我国腐植煤的还原性质及其与沉积环境的关系 |
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引用本文: | 赵师庆.我国腐植煤的还原性质及其与沉积环境的关系[J].沉积学报,1984,2(2):53-65. |
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作者姓名: | 赵师庆 |
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作者单位: | 淮南矿业学院 |
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摘 要: | 一、不同还原性腐植煤的基本特征在研究华北聚煤区东部晚古生代太原组(C3)和山西组(P11)煤性质差别及显微特征的基础上,作者认为除煤岩成分和变质程度外,还存在着影响煤质的第三个成因因素--还原性质。
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收稿时间: | 1983-01-31 |
REDUCTIVITY OF HUMIC COAL IN CHINA AND ITS RELATION TO SEDIMENTARY ENVIRONMENT |
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Institution: | Huainan College of Mining |
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Abstract: | This paper deals with an preliminary study and analysis on the relationship between the sedimentary environment of coal-bearing formations and coal-forming quality in China. These coal-dearing formations are lower Carboniferous, Middle Carboniferous,Upper Carboniferous, the Early Lower Permian,Late Lower Permian, Early Upper Permian; Upper Triassic,Lower and Middle Jurassic,Upper Jurassic-Lower Cretaceous and the Lower and Upper Tertiary. |
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