苏现波, 盛建海, 李元建. 河南山西组二1煤古泥炭沼泽的类型及演化[J]. 煤田地质与勘探, 1993, 21(2): 11-17.
引用本文: 苏现波, 盛建海, 李元建. 河南山西组二1煤古泥炭沼泽的类型及演化[J]. 煤田地质与勘探, 1993, 21(2): 11-17.
Su Xianbo, Sheng Jianhai, Li Yuanjian. THE TYPE AND EVOLUTION OF Ⅱ1 COAL SWAMP IN SHANXI FORMATION IN HENAN PROVINCE[J]. COAL GEOLOGY & EXPLORATION, 1993, 21(2): 11-17.
Citation: Su Xianbo, Sheng Jianhai, Li Yuanjian. THE TYPE AND EVOLUTION OF Ⅱ1 COAL SWAMP IN SHANXI FORMATION IN HENAN PROVINCE[J]. COAL GEOLOGY & EXPLORATION, 1993, 21(2): 11-17.

河南山西组二1煤古泥炭沼泽的类型及演化

THE TYPE AND EVOLUTION OF Ⅱ1 COAL SWAMP IN SHANXI FORMATION IN HENAN PROVINCE

  • 摘要: 河南省山西组二1煤成煤古泥炭沼泽的类型及演化可明显地分为3个区:豫北区,二1煤形成于上三角洲平原的淡水森林泥炭沼泽;豫西西部区,形成于泻湖海湾演化来的半咸水草本和森林泥炭沼泽,底部分层成煤植物为草本,煤层形成于最大海退期,结束于一次短暂的海侵;豫西中东部区,形成于潮坪演化来的淡水森林泥炭沼泽,上部分层形成于半咸水泥炭沼泽,结束于一次短暂的海侵。

     

    Abstract: The type and evolution of Ⅱ1 coal swamp of Shanxi formation(Low Permian)in Henan Province can be divided into three area clearly.In the north area,Ⅱ1 coal is formed from fresh forest peat swamp which develops from upper deltaic plain.In the west area,Ⅱ1 coal is formed under herb and forest peat swamp which is developed from lagoon and ended by a short transgression.The regression is at the middle period of coal formation.The Ⅱ1 coal forming plant of low subbed is herb.In the middle and east area, Ⅱ1 coal is formed from fresh forest peat swamp which is developed from tidal flat and ended by a short transgression.The upper subbed of Ⅱ1 coal is formed under salt peat swamp.

     

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