挤压构造带compressed structural zone简称挤压带是指主要由许多压性构造形迹组成的窄长带状构造带内岩石部分或全部呈现被搅乱的状态挤压破碎带陡立地层带steeply dipping zone 直立地层带vertical zone紧密褶皱带地层倒转带和反复冲断带等往往相伴或单独出现常有片理带劈理带和构造透镜体等挤压性构造发育在分析区域构造和划分构造体系时它与褶皱轴面等压性结构面具有同等力学意义
沿边界带发育挤压破碎带和构造透镜体。
Fault breccia and tectonic lenticles well develop along the boundary zone.
由北向南分为前缘挤压滑脱构造带、斜歪倒转褶皱—逆冲断层带和逆冲推覆岩席及叠瓦状逆冲断层带。
From north to south, several tectonic belts can be distinguished: front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.
处在挤压变形带、剪切变形带到引张变形带(及地域)中岩石所承受的构造附加静水压力有逐次变小的规律性。
There is a gradual decrease in tectonic superimposed hydrostatic pressure from compressional deformation zone through shear deformation zone to extensional deformation zone.
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