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保德矿区太原组桥头砂岩沉积特征与煤聚集
引用本文:王华,陈钟惠.保德矿区太原组桥头砂岩沉积特征与煤聚集[J].煤田地质与勘探,1995,23(2):1-6.
作者姓名:王华  陈钟惠
作者单位:中国地质大学
摘    要:根据太原组桥头砂岩(体)的沉积特征(岩性、结构、沉积构造、古流特征、平面一剖面及三维空间上的几何形态)以及该砂体对下伏m13厚煤层的冲刷样式和对上覆m11煤聚集的独特控制方式,认为它属一种特殊过渡类型的河流环境的产物,并进一步分析了同沉积期的古构造背景。

关 键 词:砂岩  沉积特征    聚集作用  河流环境

THE SEDIMENTARY CHARACTERISTICS OF QIAOTAU SANDSTONE BODY AND ITS RELATION TO COAL ACCUMULATION OF TAIYUAN FORMATION IN BAODE MINING
Wang Hua,Chen Zhonghui,Zhang Shouliang,Ma Jinxian,Wu Fadong.THE SEDIMENTARY CHARACTERISTICS OF QIAOTAU SANDSTONE BODY AND ITS RELATION TO COAL ACCUMULATION OF TAIYUAN FORMATION IN BAODE MINING[J].Coal Geology & Exploration,1995,23(2):1-6.
Authors:Wang Hua  Chen Zhonghui  Zhang Shouliang  Ma Jinxian  Wu Fadong
Institution:China University of Geosciences
Abstract:This present paper deal with the data about Taiyuan Formation(C3)coal-bearing measures of Baode mining in Hedong coalfield (NW of China),based on,in the concrete, sedimentary characteristics of Qiaotau sandstone body (lithology,textures,sedimentary structures,paleocurrents and spatial geometry).And finally,the depositional environment of Qiaotau sandstone body and its erosional pattern on m13 coal-seam (underlying).its special controlling m11 coal-seam(above)has been determined. Equally, all analysis results was emphasized the synsedimentary tectono-geodynamic setting.
Keywords:sandstone  fluvial environment  washout  coal accumulation processes  tectonic conntrol  Taiyuan formation  Baode mining  
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