1) strike-thrust structure
走滑-逆冲构造
1.
According to a field geological survey and seismic cross section interpretation, we demonstrate that the main deformational feature of the north Qaidam Basin is a strike-thrust structure.
通过本次的野外地质勘察和深部地震测线研究,证实柴达木盆地北缘的主要变形样式为走滑-挤压构造,具有挤压推覆特征的同时伴生有走滑构造,并且主要断层系统沿走向滑动的距离远大于沿倾向冲断推覆的距离,从而建立了柴北缘走滑-逆冲构造的地质模型;这对其地震解释有指导作用。
2) strike-slip thrust belt
走滑逆冲构造带
1.
Ultramicrostructure of the Mesozoic strike-slip thrust belt in eastern Jiaodong;
胶东东部中生代走滑逆冲构造带的超微构造研究
3) strike-slip and thrust nappe structures
走滑-逆冲推覆构造
4) thrusting strike slip
逆冲-走滑
5) strike-slip thrust structural belt
走滑冲断构造带
1.
Geometry and kinematics of Cenozoic right-lateral strike-slip thrust structural belt in the north margin of the Qaidam Basin.;
柴达木盆地北缘新生代右行走滑冲断构造带的几何学和运动学
6) thrust-decollement system
逆冲滑脱构造
1.
The thrust-decollement system formed the frontal margin of the massif In the Mesozoic strong structural deformation was accompanied by intense thermal activity.
大别地块自晚元古代以来主要经受了自北而南的推挤，并且发生了两次较强烈的南移运动，造成了地块前线逆冲滑脱构造体系。
补充资料：逆阪走丸
1.见"逆坂走丸"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条