泌阳凹陷在区域性引张作用下形成了典型的伸展构造样式——被不同层次断层切割成的一系列复杂断鼻、断块。
Typical extensional structural patterns, cut into a series of complex fault noses and fault blocks by faults of different levels, form under regional extension force in Biyang depression.
我国东部沉积盆地是在引张背景下形成的。盆地中边隆起、边沉降、边断裂、边沉积，构造作用与沉积作用同步发生。
The East China sedimentary basins are believed to be formed by extension rifting simultaneously with the process of uplifting, subsiding, faulting and deposition.
我国东部沉积盆地是在引张背景下形成的。盆地中边隆起、边沉降、边断裂、边沉积，构造作用与沉积作用同步发生。
The East China sedimentary basins are believed to be formed by extension rifting simultaneously with the process of uplifting, subsiding, faulting and deposition.
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