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英吉苏中新生代凹陷是在古生代逆冲推覆构造背景之上发育起来的背驮式前陆盆地。盆地的沉积作用和变形作用严格受基底参与的逆冲断层的控制。中新生代构造由北向南可划分七个带：北部斜坡带；群克─新开屏背斜带；英北向斜带；阿拉干背斜带；英南向斜带；古城墟斜坡带和罗布庄断凸带。叠瓦式逆冲断层、冲起构造、构造三角带、断展褶皱和披覆构造是英吉苏凹陷的主要变形样式。自三叠纪以来，不同时期的沉积中心自造山带向前陆方向迁移。 中新生界变形的动力学和运动学是与塔里木板块南缘活动大陆边缘的板块拼贴事件和壳内拆离缩短作用有关。
The mid-Cenozoic sags in the Yingjisu are piggyback foreland basins developed over the Paleozoic thrust nappe. The sedimentation and deformation of the basin are strictly controlled by the basement involved in the thrust fault. The Meso-Cenozoic tectonism can be divided into seven zones from north to south: northern slope zone; Group-Keping-Xinkaping anticline belt; British northward syncline zone; Aracan anticline zone; south-south syncline zone; ancient city- Zhuang off convex belt. The main deformation styles of the Yingjisu Depression are superimposed thrust faults, uplift tectonics, structural delta belt, fault fold and drape structure. Since the Triassic, sedimentary centers of different periods migrated to the foreland from the orogenic belts. The Mesozoic-Cenozoic deformation dynamics and kinematics are related to plate collage events and the intracavernous detachment and shortening of the active continental margin in the southern margin of the Tarim plate.