摘要
北京周口店地区晚古生代煤系煤层遭受过强烈的变质与变形。与华北同时期煤田相比,它独具特色:煤级达高级无烟煤,乃至接近于超无烟煤,煤层的糜棱化构造煤极其发育。作者采用薄片、扫描电镜及X衍射诸手段对煤系及煤层的变质变形特征进行了系统的研究,确定了煤变质作用发生的时间,变质作用类型和变质作用温压条件;同时探讨了煤层变形,即糜棱化作用发生时期及形成条件。
The late palaeozoic coal measures and coal seems in zhoucoudian, Beijing,have undergone strong metamorphism and deformation. Coal rank is upper-anthracite or ultra-an-thracite and the structural coal is very common.The metamorphism characteristics and deformation characteristics of coal measure and coal beds have been studied systematically from thin section, SEM and X-ray diffraction analysis. The stage and temperature-pressure condi-tion of deformation of coal are also discussed in this paper.
关键词
晚古生代
煤系
煤层
变质作用
变形作用
metamorphism
deformation
late palaeozoic
coal measures
coal seems