鲁西煤田多级滑动构造系  

ON THE MULTI-ORDER GLIDING STRUCTURAL SYSTEM IN COALFIELDS OF WESTERN SHANDONG

作　　者：吕朋菊[1] 张永双[1] 张明利[1] 卜昌森 王克有 

机构地区：[1]山东矿业学院 [2]肥城矿务局 [3]宁阳煤炭工业局

出　　处：《地质论评》1995年第6期503-508,共6页Geological Review

基　　金：煤炭基金

摘　　要：鲁西石炭二叠纪与中奥陶世之间的假整合面为本区煤田的主滑面,它与煤系中若干次一级滑面共同组成多层次多级别的滑动构造系。本文主要分析该滑动构造系特征、形成的地质构造背景以及对煤矿生产的影响。The disconformity between the Permo-Carboniferous and Middle Ordovician in western Shandong represents the principal sliding surface in the coalfields of the study area. It combines with several second-order sliding surfaces in the coal measures to form a multi-level, multi-order sliding structural system. This paper mainly analyses the features and tectonic setting of this sliding structural system and its influence on coal production.

关 键 词：煤田 滑动构造系 不整合面 煤矿床 

分 类 号：P618.110.2[天文地球—矿床学]