王海军. 永陇矿区LYL井田2号煤层顶板沉积环境及其稳定性评价[J]. 煤田地质与勘探, 2016, 44(6): 38-44. DOI: 10.3969/j.issn.1001-1986.2016.06.007
引用本文: 王海军. 永陇矿区LYL井田2号煤层顶板沉积环境及其稳定性评价[J]. 煤田地质与勘探, 2016, 44(6): 38-44. DOI: 10.3969/j.issn.1001-1986.2016.06.007
WANG Haijun. Sedimentary environment and stability evaluation of seam roof of No.2 seam in LYL Coal mine of Yonglong coal field[J]. COAL GEOLOGY & EXPLORATION, 2016, 44(6): 38-44. DOI: 10.3969/j.issn.1001-1986.2016.06.007
Citation: WANG Haijun. Sedimentary environment and stability evaluation of seam roof of No.2 seam in LYL Coal mine of Yonglong coal field[J]. COAL GEOLOGY & EXPLORATION, 2016, 44(6): 38-44. DOI: 10.3969/j.issn.1001-1986.2016.06.007

永陇矿区LYL井田2号煤层顶板沉积环境及其稳定性评价

Sedimentary environment and stability evaluation of seam roof of No.2 seam in LYL Coal mine of Yonglong coal field

  • 摘要: 为了对煤层顶板稳定性做出合理的评价,从沉积环境入手,通过顶板岩层精细划分对比、岩心精细描述、各类岩石样品的系统采集及测试分析,结合地球物理测井(包括水文测井)、抽水试验、矿井生产资料等,研究顶板沉积环境及其与工程地质、水文地质的关系。结果表明:研究区煤层顶板的沉积环境为曲流河沉积,主要发育泛滥平原沉积微相,零星的发育决口扇、点砂坝沉积微相。泛滥平原顶板岩石稳定性差,点砂坝、决口扇顶板稳定性中等。顶板直接含水层主要形成于延安组曲流河中的决口扇、点砂坝沉积微相形成的中-厚层状透镜状砂岩中;直罗组底部的砂岩含水层形成于多期河道砂岩纵向叠置形成的巨厚层状砂岩中。沉积环境不仅影响煤层顶板工程地质特征而且影响煤层顶板含水层的分布、富水性、导水裂隙带的高度等水文地质特征。

     

    Abstract: In order to make reasonable evaluation on the stability of coal seam roof, thus for mine design, equipment selection, the roof maintenance management to provide scientific basis and to ensure the safety of mine high-efficient exploitation, research from the coal seam roof depositional environment through the roof strata classification and correlation, core fine description, samples of rock mechanics analysis of the sampling and testing system combining with the geophysical well logging technology (including hydrological logging), pumping test technology, mine production data analysis technology, and so on. The coal seam roof depositional environment and the relationship between engineering geological and hydrogeological are studied. The main research area extracting seam roof belongs to the meandering river sedimentary environments, the main development sedimentary microfacies in the flood plain, the growth of sporadic crevasse splay sedimentary microfacies, point bar sedimentary microfacies, flood plain sedimentary formation of roof rock stability belongs to the poor. The point bar, crevasse splay sedimentary formation of roof rock stability belongs to the medium, the aquifer of roof mainly formed in the crevasse splay, point bar sedimentary environment, mainly for the lenticular, small range to thick bedded sandstone, J2z aquifer formed in multiphase vertical superimposed channel sand body formed by the thick layer of sand body. Sedimentary environment not only affects the engineering geological characteristics but also impacts coal seam roof aquifer distribution, water content, the height of water flowing fracture belt and so on hydrogeological characteristics.

     

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