李小彦. 神东矿区富惰质组煤的形成条件研究——惰质组分的真菌交替成因意义[J]. 煤田地质与勘探, 2005, 33(5): 1-4.
引用本文: 李小彦. 神东矿区富惰质组煤的形成条件研究——惰质组分的真菌交替成因意义[J]. 煤田地质与勘探, 2005, 33(5): 1-4.
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LI Xiao-yan. Conditions of inertinite-rich coal generation, Shendong mining area: Significance of fungal alternating origin of inerts[J]. COAL GEOLOGY & EXPLORATION, 2005, 33(5): 1-4.
Citation: LI Xiao-yan. Conditions of inertinite-rich coal generation, Shendong mining area: Significance of fungal alternating origin of inerts[J]. COAL GEOLOGY & EXPLORATION, 2005, 33(5): 1-4.
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神东矿区富惰质组煤的形成条件研究——惰质组分的真菌交替成因意义

Conditions of inertinite-rich coal generation, Shendong mining area: Significance of fungal alternating origin of inerts

    摘要
  • 摘要: 应用煤岩学分析方法,对神东矿区富惰质组煤中惰质组分的种类、含量、形态特征、真菌衍生物特征所反映的泥炭沼泽条件进行研究,揭示了真菌交替作用对惰质组分的成因意义。

     

    Abstract: By petrographic procedure of analysis, the peat and swamp conditions of inerts of inertinite-rich coal from Shendong coal mining area are researched, which reflected from the type, proportion, shape, and fungal ramification characteristics.The study results indicated the significance of fungal alternation origin of inerts.

     

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