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主办单位:煤炭科学研究总院有限公司、中国煤炭学会学术期刊工作委员会
大同煤田石炭-二叠系接触变质煤的煤岩学特征研究
  • Title

    Study on coal petrology characteristics of contact metamorphosed coal from Carboniferous-Permian in Datong Coalfield

  • 作者

    宋晓夏马宏涛李凯杰刘东娜赵金贵薛德生

  • Author

    SONG Xiaoxia MA Hongtao LI Kajjie LIU Dongna ZHAO Jingui XUE Desheng

  • 单位

    太原理工大学矿业工程学院,太原理工大学煤与煤系气地质山西省重点实验室,山西省煤炭地质115勘查院

  • Organization
    College of Mining Engineering,Taiyuan University of Technology Shanxi Key Laboratory of Coal and Coal Measure
    Gas Geology No.115 Shanxi Coal Geological Exploration Institute
  • 摘要

    大范围的岩浆岩侵入煤体严重影响了煤矿开采和煤质,为研究接触变质煤的煤岩学特征,对大同煤田3个矿揭露的3条辉绿岩岩墙及接触变质煤剖面进行了系统采样,对样品进行了镜质体反射率测定、工业分析和元素分析以及宏观煤岩特征和显微组分特征的系统观测,并对正常煤和接触变质煤的煤岩学特征参数的差异进行了识别和统计,在对显微组分的类型进行了总结归纳基础上,并对接触变质煤中显微组分的演化和识别进行了探讨。研究结果表明:大同煤田的接触变质煤的镜质体反射率通常大于1.0%,干燥基挥发分产率小于20%;严重热变煤与侵入体直接相邻或镜质体反射率大于2.0%,其宏观煤岩特征与正常煤差异显著,可分为块状焦、砾状焦、粒状焦3种类型;轻微热变煤的镜质体反射率介于1.0%~2.0%;其宏观煤岩特征与正常煤无明显差异;大同煤田接触变质煤的显微组分可分为3类,即原有组分、天然焦基质和新生成的组分;原有组分为原始煤中未热变或轻微热变的镜质组、惰质组和类质组;天然焦基质包括由镜质组和类质组转变而来的中间相小球体、镶嵌结构体、流动结构体等;新生成的组分主要为热解碳。严重热变煤的显微组分以天然焦基质为主,轻微热变煤中残余大量原有组分。



  • Abstract
    Large-scale igneous intrusions,seriously affected the coal mining process and coal quality. In order to study the Petrograpine characteristics of the conta ct metamorphosed coal,three diabase dikes and their alteration halos were sampled at three coal mines in Datong Coalfield. Vitrinite reflectance was measured and pro ximate and ultimate analyses were identified. Macroscopic and microscopic analyses were used to compare the differences of petrograpic characteristics between the u naffected coal and the contact metamorphosed coal,the macerals in contact metamorphosed coals were identified and quantitatively analyzed. Macerals were classified and their evolution process was discussed. The results show that the contact metamorphosed coal in Datong Coalfield has the vitrinite reflectance higher than 1.0% and its volatile matter yield is normally lower than 20%.The severely altered coal is immediately adjacent to the igneous intrusion or has the vitrinite reflectance higher than 2.0%,its macroscopic characteristics are significantly different from the unaffected coal,whiol can be divided into three types: massive coke,brecciated coke and granula 「coke. The slightly altered coal has the vitrinite reflectance ranging from 1.0%to 2.0%. No obvious macroscopic difference between the slightly altered coal and the una ffected coal was observed.macerals in the contact metamorphosed coal in Datong Coalfield can be divided into three types,namely remnants of original macerals,matrix of natural coke and newly formed components. The original macerals are unchanged/slightly altered vitrinite ,inertinite, and liptinite groups. The matrix of natural coke is mainly transformed by vitrinite and liptinite groups,which include mesophase spheres, mosaic structures ,and flow structures. The newly formed component is main pyrol ytic carbon. Macerals of the severely altered coal is dominated by matrix of natural coke,while the slightly altered coal mainly comprises remnants of original macerals.
  • 关键词

    辉绿岩岩墙接触变质作用煤岩学

  • KeyWords

    diabase dike; igneous intrusion; contact metamorphism; coal petrology;

  • 相关专题
  • 图表
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    • 采样点位置图与煤样镜质体最大反射率(Ro,max/%)

    图(10) / 表(0)

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