斜冲 meaning in Chinese
oblique impact
Examples
- Thrusting is the main character , so it was named as left - slip oblique - thrusting fault
但总体以逆冲为主。因此，将其称为左行斜冲断裂构造。 - There are coherent between the spread of oblique - thrusting structure , fold and fault structure . there were close relationships between oblique - thrust structure and the reverse " s " structure in the basin . both of them are result of the left oblique - thrusting
逆冲推覆构造呈斜列式形展布与盆地内的也呈斜列式反“ s ”形展布的构造具有密切关系，都属于断裂左行斜冲的产物。 - ( 4 ) through the analysis on the spread of inner structure , thickness change of strata and seismic and geological data in the southern basin of sertengshan - xitieshan , this paper discussed the response of oblique - thrust effect on basin
( 4 )通过对赛什腾? ?锡铁山南侧盆地内部构造展布、盆地内地层厚度变化以及地震地质资料分析，探讨了赛什腾? ?锡铁山斜冲断裂作用在盆地内的响应。 - Sxotf is recognized in the northern qaidam based on the analysis of structures of area . this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge , fault breccia and fault cleavage . fault hanging wall consists of sertengshan - xitieshan napple , which is distribution in dextral en echelon . fault footwall consists of youcangshan formation in neogene
本文在对赛什腾? ?锡铁山斜冲断裂详细地段构造解析的基础上，结合盆地的沉积特征、地球物理资料等对该斜冲断裂的几何学、运动学及形成时代进行了研究，论文着重探讨了赛什腾? ?锡铁山斜冲断裂的地质意义。 - ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper . the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting , which is of great theory significance for studying regional structural framwork , relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin . moreover , the result is of guidance significance for the forecast of combination gas , distributing and formation of nappe metal deposit in northern qaidam basin
( 6 )论文探讨了赛什腾? ?锡铁山斜向逆冲推覆构造的地质意义，认为赛什腾-锡铁山断裂斜冲作用是印度板块与欧亚板块碰撞、会聚的远程效应的结果，该认识对于研究柴北缘区域构造格局、盆山关系以及更大尺度的断裂带或造山带的斜向逆冲作用具有理论意义，对柴达木北缘的油气预测、推覆体金属矿床的分布、形成具有指导意义。