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杨树沟和卧虎沟地区北票组沉积特征

Sedimentary characteristic of Beipiao formation of Yangshugou and Wohugou districts

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【作者】 闫剑飞朱志敏王宇林

【Author】 YAN Jian-fei, ZHU Zhi-min, WANG Yu-lin (College of Resource and Environment Engineering, Liaoning Technical University,Fuxin 12300,China)

【机构】 辽宁工程技术大学资源与环境工程学院辽宁工程技术大学资源与环境工程学院 辽宁 阜新 123000辽宁 阜新 123000辽宁 阜新 123000

【摘要】 运用沉积学理论,阐述了辽西喀左杨树沟和卧虎沟地区北票组由河流体系、湖泊体系构成;进而分析了河道相、河岸相、泛滥盆地相和滨浅湖相、湖泊三角洲相(包括分流河道、沼泽及泥炭沼泽、间湾、河口坝和远砂坝、前三角洲等成因类型)、深湖相及浊积相的主要特征;重塑了该区北票组沉积环境演化史及聚煤环境;最后,指出卧虎沟地区北票组是今后找煤的重点地区。

【Abstract】 Applying sedimentological theory, the article formulated that the Beipiao formation of Yangshugou and Wohugou districts is composed of fluvial system and lacustrine system; then analysed the main characteristic of stream channel facies, stream bank facies, flood basin facies, coastal shallow-lake facies, lake delta facies(including such genetic types as distributary channel, marsh and peat swamp, interdistributary bay, mouth bar and distal bar, and prodelta), deep-lake facies and turbidite facies; it remoulded Beipiao formation depositional enviroment evolution and coal-forming environment in this district, and at last, it pointed out that Wohugou district is the main coal-exploring district.

  • 【文献出处】 辽宁工程技术大学学报 ,Journal of Liaoning Technical University , 编辑部邮箱 ,2003年S1期
  • 【分类号】P512.2
  • 【被引频次】1
  • 【下载频次】78
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