刘钦甫. 湖南测水组粘土矿物组合及其环境意义[J]. 煤田地质与勘探, 1990, 18(1): 14-17.
引用本文: 刘钦甫. 湖南测水组粘土矿物组合及其环境意义[J]. 煤田地质与勘探, 1990, 18(1): 14-17.
The Clay Mineral Association and Enviromental Significance of Ceshui Formation in Hunan Province[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 14-17.
Citation: The Clay Mineral Association and Enviromental Significance of Ceshui Formation in Hunan Province[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(1): 14-17.

湖南测水组粘土矿物组合及其环境意义

The Clay Mineral Association and Enviromental Significance of Ceshui Formation in Hunan Province

  • 摘要: 测水组粘土矿物主要为高岭石及伊利石,其次为少量绿泥石、叶腊石及伊利石一蒙脱石混层矿物。它们在垂向上具有一定变化规律,与沉积环境的演化相一致。泻湖及演浅海沉积中粘土矿物主要为伊利石和绿泥石.潮坪、淡水泻湖及沼泽沉积中主要为高岭石,其次为伊利石。

     

    Abstract: The Clay Mineral Association and Environmental Significance of Ceshui Formation in Hunan Province一Clay minerals in Ceshui formation are cormposed mainly by kaolinite and illite, and secondarilv by a little of chlorite, pyrophyllite and illite-montmoril-lonite mixing layers. These minerals show regu lar. vertical variation, which. Corresponds to the evoluation of sedimentary environments.Illite and pyrophyllite are prevailing in lagoon and littoral shallow deposits. Koalinile and illite are respectively major and secondary clay minerals in fresh lagoon and swamp deposits.

     

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