中国泥盆纪煤煤岩研究  

COAL PETROLOGICAL STUDY OF CHINA DEVONIAN COAL

作　　者：程顶胜[1] 韩德馨[1] 王延斌[1] 肖贤明 盛国英 

机构地区：[1]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

出　　处：《煤田地质与勘探》1995年第1期25-28,T001,共5页Coal Geology & Exploration

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。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.

关 键 词：角质残植煤 泥盆纪 煤级 煤岩 岩石成分 

分 类 号：P618.110.4[天文地球—矿床学]