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在柴达木盆地的侏罗系中，鉴别出了两种指示前陆盆地动力过程的构造层序：一种是响应于造山带逆冲加载过程的弹塑性转换沉降型构造层序；另一种是响应于基底塑性回沉过程的塑性回沉型构造层序。柴达木盆地的侏罗系共出现了８个构造层序：下侏罗统普林斯巴阶至中侏罗统巴柔阶４个弹塑性转换沉降型构造层序；中侏罗统巴通阶至卡洛阶下部２个塑性回沉型构造层序；中侏罗统卡洛阶上部和上侏罗统２个弹塑性转换沉降型构造层序。这种充填序列表明侏罗纪的柴达木盆地经历了多旋回弹塑性转换沉降、总体塑性回沉和再次弹塑性转换沉降３个演化阶段。此演化过程与同期造山带的隆升和向前陆带的逆冲加载过程密切相关。
In the Jurassic of the Qaidam Basin, two tectonic sequences indicating the dynamics of the foreland basin have been identified: one is an elasto-plastic transitional subsidence tectonic sequence that responds to the thrust loading of the orogenic belt; the other Species are plastic subsidence-type tectonic sequences that respond to the plastic dullback process of the basement. There are eight tectonic sequences in the Jurassic of the Qaidam Basin: four elasto-plastic transitional subsidence tectonic sequences from the Lower Jurassic to the Middle Jurassic, Barins Step; Middle Jurassic There are two plastic subsidence-type tectonic sequences from the middle to the lower Carlo scale, and two elasto-plastic transposed sedimentary-type structural sequences in the Upper Carono-Upper Middle Jurassic and Middle Jurassic. This filling sequence indicates that the Jurassic Qaidam Basin experienced three stages of evolution: multi-cycle elastoplastic transformation, total plastic recovery and elasto-plastic transition. This evolutionary process is closely related to the uplift of the orogenic belt and the thrust loading of the foreland belt in the same period.