| 中国泥盆纪煤煤岩研究 |
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| 引用本文： | 程顶胜,韩德馨.中国泥盆纪煤煤岩研究[J].煤田地质与勘探,1995,23(1):25-28,T001. |
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| 作者姓名： | 程顶胜 韩德馨 |
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| 作者单位： | 石油大学，中国矿业大学北京研究生部，中科院地化所广州分部 |
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| 摘 要： | 中国泥盆纪煤是形成于一定地质历史条件下的特种煤、显微组成以富含角质本为特征，其它壳质组分、镜质组、惰性组含量均低。泥盆纪煤阶的确定可用角质体荧光参数、角质体反射率及富氢镜质组的反射率。
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| 关 键 词： | 角质残植煤 泥盆纪 煤级 煤岩 岩石成分 |
COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL |
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| Cheng Dingsheng, Han Dexin, Wang Yanbin.COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL[J].Coal Geology & Exploration,1995,23(1):25-28,T001. |
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| Authors: | Cheng Dingsheng Han Dexin Wang Yanbin |
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| Abstract: | hina Devonian coal is a special kind of coal which was formed under certain geological historical conditions. Microscopically, it is rich in cutinite but has a low content of other exinites, vitrinite and inertinite respectively. The coal rank of Devonian coal can be determinated by fluorescence parameter and reflectance of eutinite and hydrogen--rich vitrinite. |
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| Keywords: | cutinite liptobialith Devonian macerals rank cutinite reflactance |
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