1) Strike-slip Structural SystX
走滑构造体系
2) Strike-slip structure
走滑构造
1.
Characteristics of strike-slip structure and rules of hydrocarbon accumulation in northern Liaodong Bay;
辽东湾北部地区走滑构造特征与油气富集规律
2.
The geometry (type, classification, assemblage) , forming period-times and genesis mechanism of the strike-slip structures in the eastern Jiyang Depression have been researched in this paper using structural analytic method to gain more knowledge of the strike-slip structures.
为了提高走滑构造的研究程度,将济阳坳陷东部作为一个整体,应用构造解析方法,研究其走滑构造的形态、分类、组合形式及形成期次并探讨了其成因机制。
3.
The weaknesses, difficulties and key points of the present study of basin tectonic dynamics are shown in the following four aspects: (1)Tectonics with complex features and complex cause of formation, such as strike-slip structure, lateral trans.
目前盆地构造动力学研究的弱点、难点及重点主要有以下4方面:(1)特征或成因复杂的构造,如走滑构造、横向(转换)构造、拆离滑覆构造、较大型断层的分段性和断裂带的结构等。
3) Punda strike-slip faults
Punda走滑构造
1.
According to the characteristics of master fault and its secondary strike-slip faults of the Punda strike-slip faults, we know the collision between Luconia continent and Sundaland and strike-slip of Lupar valley are predominant dynamic process in the formation of the Punda strike-slip faults.
沙捞越Punda走滑构造为一典型的右旋走滑构造形式,是沿近东西向F断裂(PDZ)发育特征的负花状构造或郁金香构造,并构成走滑伸展双重构造。
4) gliding structure system
滑移构造体系
5) 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。
6) strike-slip inversion
走滑反转构造
补充资料：多字型构造体系
见直扭构造体系。
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