肥城煤田滑动构造的发现及其意义  

THE DISCOVERY OF GLIDING TECTONICS IN FEICHENG COALFIELD AND ITS SIGNIFICANCE

作　　者：吕朋菊 魏久传 张明利 

机构地区：[1]山东矿院地质系

出　　处：《山东矿业学院学报》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

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

关 键 词：煤田 滑动构造 断块活动 

分 类 号：P618.110.2[天文地球—矿床学]