摘要
吐谷鲁背斜位于新疆准噶尔盆地南缘西部山前霍玛吐构造带。立足于现代构造地质学理论新进展对山前复杂构造带的构造解释,主要运用断层相关褶皱理论根据地震资料进行构造建模,推断吐谷鲁背斜构造的主要构造样式为早期深部构造楔与后期突破推覆构造的叠加组合。最终运用三维可视化成图软件形成直观的构造解释三维图,方便进一步分析。
Tugulu anticline is located at the complicated foreland structure zone in the south margin of Junggar Basin,XinJiang province.This study is aimed at a better structure elucidation with the help of modern tectonics in complicated foreland zone.fault-related theories are mainly used in dealing with seismic data to carry on structure modeling.Finally,the conclusion that the structure pattern of Tugulu anticline is composed by an earlier deep duplex tectonic wedge and a latter broke out thrust overlaying.There will be some 3D visualized pictures of tectonics interpretation made by 3D visualized restitution software which can help us to do some more analyses.
出处
《西南石油大学学报（自然科学版）》
CAS
CSCD
北大核心
2007年第S2期9-11,167-168,共5页
Journal of Southwest Petroleum University(Science & Technology Edition)
关键词
断层相关褶皱
构造楔
三维成图
fault-related folds
tectonic wedge
3D visualized restitution
