夏文臣, 要庆军, 初志民, 贾春. 黔西晚二叠世含煤岩系中潮坪-潮道相沉积构成及环境解释[J]. 煤田地质与勘探, 1988, 16(5): 2-11.
引用本文: 夏文臣, 要庆军, 初志民, 贾春. 黔西晚二叠世含煤岩系中潮坪-潮道相沉积构成及环境解释[J]. 煤田地质与勘探, 1988, 16(5): 2-11.
shu
Sedimentary Constituent and Environmental Interpretation of Tidal Flat-Tidal Channel Facies in Late Permia Coal-Bearing Formation, West of Guizhou Province[J]. COAL GEOLOGY & EXPLORATION, 1988, 16(5): 2-11.
Citation: Sedimentary Constituent and Environmental Interpretation of Tidal Flat-Tidal Channel Facies in Late Permia Coal-Bearing Formation, West of Guizhou Province[J]. COAL GEOLOGY & EXPLORATION, 1988, 16(5): 2-11.
shu

黔西晚二叠世含煤岩系中潮坪-潮道相沉积构成及环境解释

Sedimentary Constituent and Environmental Interpretation of Tidal Flat-Tidal Channel Facies in Late Permia Coal-Bearing Formation, West of Guizhou Province

    摘要
  • 摘要: 为了更有效地识别沉积相和重建含煤岩系沉积环境,我们在野外工作中,除了详细观察描述和解释沉积构造和其它成因标志外,还侧重研究了各类沉积体的几何学特征和内外沉积构成。利用陡坎或沟谷切割的自然断面测绘详细沉积断面图。在断面图上划分成因地层单位,研究各成因地层单位的沉积构成及含煤性,并对其进行成因分析。

     

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