裂陷作用也控制着弧后盆地的形成。
Rifting played an important role in formation of the back arc basins.
这种四元结构的形成，起因于区域构造应力场转变成裂陷作用、拗陷作用和差异隆升反转作用的演化。
This four-element architecture may be caused by a regional stress field evolution from rifting, sagging to differential inversion uplifting.
盆地形成机制研究在深部过程控制、多重机制联合作用、幕式裂陷和反转过程等方面取得显著进展。
Recent studies have further improved our understanding of basin forming mechanism in deep processes, combined mechanism and multiple rifting and inversion.
这两种构造系统是盆地区新生代时期主动裂陷和被动裂陷两种作用机制的具体表现。
The two tectonic systems are concrete manifestations of the active rifting and passive rifting mechanisms in the basin during the Cenozoic.
区域地壳拉张作用下盆地的阶段性裂陷，会导致边界断裂的多期活动和山地的相对隆升。
Regional crust pulling-apart induces sinking of basin, resulting in multi-periodic activities of boundary faults and relative uplifting of mountain.
多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构。
Complicated tectonic styles and geological structures were generated by multi-episodic rifting and inversion.
多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构。
Complicated tectonic styles and geological structures were generated by multi-episodic rifting and inversion.
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