摘要
首次提出了肥城煤田石炭二迭系与奥陶系之间假整合面上存在重力滑动构造;论述了其存在依据,对其特征进行了初步研究,并探讨了其成因及其对煤矿生产的影响。肥城煤田重力滑动构造的发现,对今后在鲁西各煤田开展滑动构造的研究将起到重要的启示和指导作用。
This paper, for the first time, proposes the existence of gliding tectonics on the disconformity plane between the Permo Carboniferous coal measures and Ordovician limestons in Feieheng coalfield, presents a preliminary study to its characteristics and goes further into its origin. The discovery of the gliding tectonics in Feicheng coalfield will give a good deal of enlightenment and guidance to the study of this kind of structure in coalfields of Western Shandong
出处
《山东矿业学院学报》
CAS
1992年第2期120-126,共7页
Journal of Shandong University of Science and Technology(Natural Science)
基金
煤炭科学基金
关键词
煤田
滑动构造
断块活动
: fault-block movement
fracture
unconformaty
microstructure
