• 责任者：Yu Jingdu (State Key Laboratory of Oil and Gas Reservoir Geology and Exploration ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Zhongquan
• 刊名：Journal of Chengdu University of Technology
• 出版年：2012
• 卷期：39(3)
• 关键词：滑脱构造 ; decollement ; 龙门山断裂带 ; Longmenshan Fault Zone
• 页码：p.305-310
• 图表：3 illus., 1 table, 16 refs.
• 分类号：0300
• issnNo：ISSN1671-9727
• isbnNo：CN51-1634/N

///This paper studies the mechanism of the tectonic dynamics in forming the Longmenshan structural belt in the early stage of the late Indo-Sinica epoch and the possibility of forming the local compressive environment. Through the simulation experiment in which the main power is gravity, it indicates that gravitational sliding can emerge under the background of differential upheaval in the plate and there exists the possibility of forming a compressional structure in the front of the sliding body. The formation of the Longmenshan tectonic zone is considered to be the stacked thrusting process after experiencing the extensional structure.