- 责任者：Yang Yuanyu (College of the Earth Sciences ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Zhongquan
- 刊名：Petroleum Geology & Oilfield Development in Daqing
- 出版年：2013
- 卷期：32(1)
- 关键词：构造演化 ; structural evolution ; 龙门山 ; Longmen Mountains
- 页码：p.12-17
- 图表：illus., 17 refs.
- 分类号：0300
- issnNo：ISSN1000-3754
- isbnNo：CN23-1286/TQ
By the studies of the commingled interpretation and the structural evolution of the seismic profiles, Fengshunchang-Tianjing Mountain Tectonics has experience, the following three evolution process from Sinian to Now. extended to generate a basin, gravity gliding and compressional orogenesis under the background of the conti- nental uplift and expansion. At the extensional basin stage （Z-T2）, there were no Fengshunchang-Tianjing Moun- tain structures, but sedimentated a series of sea facies carbonate and clastic formations. At the gravity gliding stage （ T3-J2 ） , located in the front of the gravity gliding belt of the structural system, Fengshunchang-Tianjing Mountain regionally developed into a series of thrust nappe structures taking thin surface structure as the main form; since Late Jurassic period （J3-Q） , the compressional orogenesis has formed, the background of the structural dynamics changes gradually from stretching/gravity gliding to horizontal compression, accompanied with the basement-in- volved deformation, and then a series of advance thrust structures taking thick surface structure as main form are produced. After eroding, the above structures manifests as nowaday structural patterns.