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色力布亚断裂系是塔里木盆地西南坳陷与巴楚隆起两大构造单元的分界线。该断裂系由两条北北西向斜列的右行走滑挤压基底断裂和一系列位于基底断裂重叠区内的盖层滑脱逆冲断层组成，剖面上可以分成两种不同层次的构造样式：深层为基底卷入的走滑逆冲构造；浅层为第四系继承性滑脱构造。两条边界断裂带的活动是导致内部复杂构造的主要原因，各断裂与逆冲席共同组成一个统一的走滑双重构造。根据沉积及内部变形特征，该构造带的演化分为４个阶段，即三叠纪边界走滑断裂形成阶段、渐新世进一步发育阶段、上新世强烈变形阶段和第四纪不均衡活动阶段。
The Seleuya fault system is the dividing line between the two major tectonic units in the southwestern depression and Bachu uplift in the Tarim Basin. The fault is composed of two strike faults of the right-lateral strike-slip crush and a series of capstones detachment and thrust faults located in the overlap zone of the basement faults. The faults can be divided into two different levels of structural styles: deep As the basal strike slip thrust structure; the shallow layer of the Quaternary successional slippage structure. The activities of the two boundary faults are the main causes of the complicated internal structures. Each of the faults and the thrust mat together form a unified dual structure of strike-slip. According to the characteristics of sedimentation and internal deformation, the evolution of the tectonic belt is divided into four stages, that is, the Triassic boundary strike-slip fault formation stage, the Oligocene further development stage, the Pliocene strong deformation stage and the Quaternary Uneven Activity stage .