程顶胜, 韩德馨, 王延斌, 肖贤明, 盛国英. 中国泥盆纪煤煤岩研究[J]. 煤田地质与勘探, 1995, 23(1): 25-29.
引用本文: 程顶胜, 韩德馨, 王延斌, 肖贤明, 盛国英. 中国泥盆纪煤煤岩研究[J]. 煤田地质与勘探, 1995, 23(1): 25-29.
Cheng Dingsheng, Han Dexin, Wang Yanbin, Xiao Xianming, Sheng Guoying. COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL[J]. COAL GEOLOGY & EXPLORATION, 1995, 23(1): 25-29.
Citation: Cheng Dingsheng, Han Dexin, Wang Yanbin, Xiao Xianming, Sheng Guoying. COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL[J]. COAL GEOLOGY & EXPLORATION, 1995, 23(1): 25-29.

中国泥盆纪煤煤岩研究

COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL

  • 摘要: 中国泥盆纪煤是形成于-定地质历史条件下的特种煤,显微组成以富含角质体为特征,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。

     

    Abstract: China 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 incrtinite 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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