摘要
根据地震资料、钻井和野外调查等研究,认为天井山构造带广泛发育重力滑动构造、断层转折褶皱、倒转背斜和双重构造等构造样式.天井山构造带变形具有垂向分层特点:上部构造主要为断层转折褶皱,02tjs10测线附近变形强度最大,向两端变形逐步减弱;下部构造为多个逆冲岩片叠置所构成的双重构造.通过构造物理模拟实验,证实天井山构造带在北西—南东向挤压应力作用下变形序列为前展式逆冲叠瓦式构造组合;天井山构造带存在多个滑脱层系,才会形成分层变形、垂向叠置的不协调收缩构造变形.该研究可以为天井山构造带乃至龙门山油气勘探提供指导.
According to the comprehensive study of the earthquake and field surveys,Tianjing mountain Tectonic zone has wide range of developmental of structural styles such as gravitational gliding tectonics,fault-bend fold,overturned anticline and dual structure.The deformation characteristics of Tianjing mountain Tectonic zone is vertical stratification.By the construct physical simulation experiments,proving that the Tianjing mountain tectonic zone thin-skinned structure which developed in Indosinian is controlled by south-north compressive stress and northwest-southeast gravity gliding.In the Himalayan period,the deformation sequence of Tianjing mountain tectonic zone is piggy-back thrust imbricate structure combination controlled by south-north compressive stress.The Tianjing mountain tectonic zone has more than one detachment systems.In the decollement,there are hierarchical deformation and vertical stacking of uncoordinated contraction of tectonic deformation formed.
出处
《东北石油大学学报》
CAS
北大核心
2012年第6期1-7,共7页
Journal of Northeast Petroleum University
基金
国家自然科学基金重点项目(41030426)
四川省青年科技基金项目(03ZQ026-046
05JY029-088-2)
关键词
龙门山北段
天井山
物理模拟
造山过程
挤压应力
滑脱层系
构造样式
north part of Longmen mountain
Tianjing mountain
physical simulation
orogenic processes
compressive stress
detachment layer systems
detachment systems
structural style
