鲁西中新生代复合伸展构造系统  

The Compound Extension Structure System of Meso-Cenozoic in West Shandong Province

作　　者：王桂梁[1] 燕守勋[1] 姜波[1] 

机构地区：[1]中国矿业大学煤田地质系

出　　处：《中国矿业大学学报》1992年第3期1-12,共12页Journal of China University of Mining & Technology

基　　金：国家自然科学基金资助

摘　　要：鲁西地区由铲式断层、转化断层及深浅不同的滑脱断层共同组合成连锁断层系统;结合晚侏罗统到早第三系的沉积相系及岩浆活动所反映的伸展历程及其动力机制,可建立一个我国特有的多层次、多滑面、多种断层组合、多向伸展的,并以泰山、鲁山、沂山和尼山为伸展隆升体的复合伸展构造系统。The linked system of faults has been composed of the listric. transfer faults, and the decollement faults with different buried depths in West Shandong Province. In combination with the extensional process and dynamic mechanism reflected by sedimentary facies and magma action from Late Jurassic to Eogene. a compound extension structure system characterized by multi-levels, multiple glide surface, multiple pattern, multi-directional extension, and extensional upwarped bodies of Taishan -Lushan-Yishan and Nishan mountains has been established.

关 键 词：鲁西 中新生代 伸展构造系统 

分 类 号：P547[天文地球—构造地质学]