陈荣舟. 水城矿区龙潭组浅绿色泥岩的特征及成因[J]. 煤田地质与勘探, 1990, 18(1): 17-20.
引用本文: 陈荣舟. 水城矿区龙潭组浅绿色泥岩的特征及成因[J]. 煤田地质与勘探, 1990, 18(1): 17-20.
Features and Genesis of the Light-green Mudstones of Longtan Formation in Shuicheng Mining Aaea[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 17-20.
Citation: Features and Genesis of the Light-green Mudstones of Longtan Formation in Shuicheng Mining Aaea[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 17-20.

水城矿区龙潭组浅绿色泥岩的特征及成因

Features and Genesis of the Light-green Mudstones of Longtan Formation in Shuicheng Mining Aaea

  • 摘要: 水城矿区龙潭组二段下部赋存的两层浅绿色泥岩(粘土化凝灰岩),特征显著,分布稳定。通过对其进行宏观观察、镜下鉴定、化学分析,差热分析、X 射线衍射分析等综合研究,认为它主要由火山物质在沼泽-近海湖泊里沉积而成,可以作为矿区和区域煤层对比的可靠标志层。

     

    Abstract: Features and Genesis of The Light-green Mudstones of Longtan Formation in Shuicheng Mining Aaea——In the cower of the second section of Longtan formation there are two light-green mudstones (clayey tuff) with evident features and stable distribution. The Combining study using macroscopic and microscopic examination, Chemical, differeatial theamal nad X-diffraction analysis indicates that the muds-tones were formed composed of volcanic materials ceposited in marsh and coastal larkes. The mudstones Can be used as reliable marker for seam Correlation in the mining area and the region.

     

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