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贵州织金煤矿区龙潭组岩石特征及其意义

ROCK CHARACTERISTICS OF LONGTAN FORMATIONOF ZHIJIN COAL-MINE IN GUIZHOU AND ITS SIGNIFICANCE

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【作者】 陶述平谭西德黄昔容

【Author】 TAO Shu-pingTAN Xi-deHUANG Xi-rong (Xiangtan Polytechnic University, Xiangtan Hunan 411201, China)

【机构】 湘潭工学院湘潭工学院 湖南湘潭411201湖南湘潭411201湖南湘潭411201

【摘要】 织金矿区含煤地层为上二叠统龙潭组,含主要可采煤层。煤系地层以含玄武岩屑、 6海绿石为特征的类碎屑岩夹碳酸盐岩,水平、沙纹、波状层理发育,煤系中稳定的灰岩、硅铁5质灰岩标志层较多,有利于煤层的划分与对比,并产丰富的动植物化石及碎块。属海、陆交替环境下的标型海陆交互相沉积。

【Abstract】 Stratum containing coal of Longtan Formation in Zhijin mine zone include mainly 6 layers of coal that can be picked. In coal beds, five sorts of clasolite with the characteristics of basalt bits and glauconite mixed with carbonate, bedding development of horizon, sand-vein, wave-shape, and lots of key beds of steady (silicon-iron) limestone, favour division and comparison. Plentiful zoolite and phytolite and fragment occur also in the coal bed. This bed belongs to typomorphic paralic deposition under paralic circumstance.

  • 【分类号】P618.11
  • 【被引频次】9
  • 【下载频次】286
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