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论证了青藏高原形成与隆升过程中的变形构造格局。岩石圈结构、青藏高原隆升与周边前陆沉积盆地耦合关系、高原隆升的地球动力学模式等。提出青藏高原碰撞-隆升过程中，高原边缘以走滑-挤压构造为主，高原内部以伸展构造为主；高原隆升过程中，岩石圈变形总体是：上部以伸展变形为主，中部以挤压变形为主，下部以伸展变形为主。通过青藏高原及周边岩石圈结构及隆升过程变形作用时-空耦合关系的对比研究，建立起青藏高原隆升机制的多向碰撞-入隆升地球动力学模式。
Demonstration of the tectonic deformation pattern during the formation and uplifting of the Qinghai-Tibet Plateau. Lithospheric structure, the coupling between the uplift of the Qinghai-Tibet Plateau and the surrounding foreland sedimentary basins, and the geodynamic model of plateau uplift. It is suggested that during the collision-uplift of the Qinghai-Tibet Plateau, the strike-slip-extrusion structure is the main edge of the plateau and the extensional structure is dominant in the interior of the plateau. During the uplift of the plateau, the deformation of the lithosphere is generally dominated by extensional deformation in the upper part, To squeeze the main deformation, the lower part of the main deformation and extension. The multi-directional collision-uplift-up geodynamic model of the uplift mechanism of the Qinghai-Tibet Plateau is established through the comparative study of the time-space coupling relationship between the lithosphere structure of the Qinghai-Tibet Plateau and its surrounding and the deformation process of uplift.