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贵州大竹坝井田含煤地层及煤层特征分析
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摘要
介绍了贵州省桐梓县大竹坝井田地质概况、构造特征和煤层赋存情况,分析了井田内含煤地层及可采煤层特征,阐述了煤层特征及其变化规律。研究表明,井田内含煤地层为上二叠统龙潭组,可采煤层3层,其中C3为主采煤层,C2、C4零星局部可采。井田内C3煤层厚度变化规律不明显,煤类单一,煤层结构较简单,属于较稳定类型煤层;估计探明煤炭资源量8339万t,为一中型井田;根据煤质化验结果,确定C3煤层煤岩的工业类型为中灰、中高硫、低磷、高热值贫瘦煤。
        Geology,structure characteristics and occurrence of coal seams in Dazhuba coal field in Tongzi county of Guizhou province were introduced,the coal-bearing strata and coal seam characteristics were analyzed,and the characteristics and change rule of coal seams were elaborated.The results showed that the coal-bearing strata of Dazhuba coal field so the C3 coal seam was the Longtan formation of the Upper Permian series,it had 3 minable seam,and C3 coal seam was the main minable seam,while C2 and C4 seams were partly minable.The thickness variation of C3 coal seam was not obvious,there was a single type of coal and the structure of seam was relatively simple,So the C3 coal seam was a relatively stable coal seam.Its estimator of proven coal resources was 83.39 million tons,which was a mediumsized coal field.According to coal quality laboratory test results,the industrial type of C3 coal was characterized by meager lean coal with medium ash content,medium-high sulfur content,low phosphorus content and high calorific value.
引文
[1]洪秀萍,吕帅,梁汉东.贵州省“西电东送”存在的问题及对策[J].煤炭技术,2015(10)
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    [4]阚小波.物探数字测井在黔北水柴坝井田勘查中的应用效果[J].煤炭技术,2014(11)
    [5]张有河,王晓明,刘东娜.准格尔煤田西南部6上煤层煤岩煤质及沉积环境特征[J].中国煤炭,2015(2)
    [6]廖友常,雷志远,翁申富等.贵州省桐梓县洪村坝-大竹坝煤矿大竹坝井田勘探地质报告[R].贵州省地矿局106地质大队,2006
    [7]廖友常.桐梓大竹坝井田C3煤层理化特征及工艺性能[J].贵州地质,200/(1)
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