thrust structure meaning in Chinese
承受推力结构
发动机架
Examples
- It is concluded that the thrust structure formed in late - jurassic . faults with high angles appeared in hengshanbu structure part which is also developed in late - jurassic deduced by strata contact relationship . middle district includes two parts which
横山堡构造带发育由东向西逆冲的高角度断裂，根据地层接触关系，推断该构造带的逆冲活动发生于晚侏罗世。 - 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。 - Kongxi buried hill shows following features in the seismic profiles : the structures are asymmetric . there is flexural syncline on the east side and a monocline on the west side . asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle . the permo - carboniferous system of both sides almost lie in the same slope and the events of cambrian or upper proterozoic are continuous from east to west . the phenomenas suggest that kongxi buried hill could be a thrust belt been traced which consists of reverse faults . the imbricate faults mainly effect pre - jurassic strata . there are obvious angular unconformity between jurassic - cretaceous system and paleozoic involved deformation of thrust . the thrust front in some place has cut off the beds of jurassic - cretaceous system . the structural style of the thrust structure changes along the strike of the kongxi buried hill
地震和钻井资料揭露的孔西构造带前第三系潜山的地质特征可以归纳为：构造带总体上不对称构造带内部有地层重复现象石炭二叠系地层的位置明显高于两侧的同一地层的高度。用由34条向东倾斜的逆冲断层组成的叠瓦扇构造模式能够比较合理地解释上述地质特征。该带向东倾斜的逆冲叠瓦状断层组主要影响前侏罗系地层，侏罗白垩系与卷入逆冲构造变形的古生界地层之间有明显的角度不整合。 - ( 5 ) according to the study on seismicic data , sedimentary characteristics , contact relations , incision relation of the faults and strata related to the folds which are associated with the faults , this paper reached the conclusions : the oblique - thrusting structure of sertengshan - xitieshan in northern qaidam basin was formed in middle jurassic and the left - thrusting fault zone was established in the late pliocene of neogene
( 5 )根据地震质料、沉积特征、地层的沉积接触关系、断裂切割地层关系以及与断裂相关的褶皱卷入地层的研究，认为柴达木盆地北缘的赛什腾? ?锡铁山逆冲推覆构造形成于中侏罗世，而左行逆冲断裂带定型于新第三纪上新世末。