王运泉, 孟凡顺. 义马煤田义马组砂岩中镜煤化直立树干的成因及环境意义[J]. 煤田地质与勘探, 1987, 15(4): 15-16.
引用本文: 王运泉, 孟凡顺. 义马煤田义马组砂岩中镜煤化直立树干的成因及环境意义[J]. 煤田地质与勘探, 1987, 15(4): 15-16.
Genesis and Environment Significance of Vit-rinizated Vertical trunks in the Sandstone in Yima Formation,Yima Coal Field[J]. COAL GEOLOGY & EXPLORATION, 1987, 15(4): 15-16.
Citation: Genesis and Environment Significance of Vit-rinizated Vertical trunks in the Sandstone in Yima Formation,Yima Coal Field[J]. COAL GEOLOGY & EXPLORATION, 1987, 15(4): 15-16.

义马煤田义马组砂岩中镜煤化直立树干的成因及环境意义

Genesis and Environment Significance of Vit-rinizated Vertical trunks in the Sandstone in Yima Formation,Yima Coal Field

  • 摘要: 义马煤田义马组含煤岩系是一套典型的陆相沉积,岩性、岩相横向变化大。众所周知,在煤层底板中,直立树干化石是屡见不鲜的,但砂岩中存在有众多的直立树干化石且大部分都镜煤化实属少见。笔者在对义马组环境分析过程中注意了这一现象并对其成因和环境意义作了探讨。

     

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