黔西柏杨井田含煤岩系沉积环境与聚煤规律

Sedimentary Environment and Coal Accumulation Law of Coal Bearing Rock Series in Baiyang Well Field of Qianxi

  • 摘要: 针对柏杨井田的研究大多集中于矿井地质方面,对井田地质成因方面的研究相对薄弱,不利于下步煤炭资源勘查工作的顺利展开问题,运用沉积相分析的方法和原理,对典型含煤岩系钻孔剖面进行了系统的沉积相分析。结果显示,该区含煤岩系沉积环境从下到上依次为潟湖-潮坪、三角洲平原、潟湖-潮坪,三角洲平原聚煤作用最优,沉积了该区主要的可采煤层M2、M4、M5、M9;除古地理条件外,古植物、古气候、古构造条件也是聚煤的重要控矿因素,共同控制了聚煤作用的发生和煤炭资源的保存。研究成果可为该区下步煤炭的资源勘查提供相应的理论指导。

     

    Abstract: Aiming at the problem that most of the research on Baiyang Well Field focuses on the geological aspects of the mine,and the research on the aspect of well field geological genesis is relatively weak,which is not conducive to the smooth development of the next step coal resources exploration work.Utilizing the method and principle of sedimentary facies analysis,a systematic sedimentary facies analysis is conducted on the borehole sections of typical coal bearing rock series.The results indicate that the sedimentary environment of the coal bearing rock series in the area,from bottom to top,there are lagoon-tidal flat,delta plain,and lagoon-tidal flat.The delta plain has the best coal accumulation action and deposits the main mineable coal seams M2,M4,M5,and M9 of the area;Except for the ancient geographical conditions,ancient plants,ancient climate,and ancient structural conditions are also significant ore-controlling factors for coal accumulation,which jointly control the occurrence of coal accumulation action and the preservation of coal resources.The research results can provide corresponding theoretical guidance for the resource exploration of next step coal in the area.

     

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