摘要
滕南煤田的煤层挥发份变化在纵向上具有反希尔特定律的规律；在横向上具有南低北高的特征，主要从成煤环境角度，探讨了上述规律的成因。
The change of volatile in Tengnan coad field has the phenomenon of anti Hilt law in vertical direction and the trend of increase from the south to the north in horizontal direction. The article probes into the cause from the coal forming environment.
出处
《山东矿业学院学报》
CAS
1997年第2期163-168,共6页
Journal of Shandong University of Science and Technology(Natural Science)
关键词
挥发份
镜质组
成煤环境
煤层
volatile
vitrinite
coal forming environment
