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主要基于火成岩组合讨论了大地构造演化。提出碰撞型蓝片岩是大洋闭合与陆－陆碰撞作用的产物和标志，白云母／二云母花岗岩是陆内俯冲作用的岩石学记录，以钾玄岩系列为主的火成岩组合是水平缩短式陆内造山带边界的标志，造山末期Ａ型花岗岩是造山带崩塌的标志。重建了祁连山—柴达木地区与北山地区的构造演化和造山过程。讨论了新生代陆内造山－岩浆作用，提出了青藏－喜马拉雅陆内造山火成岩的成对性，由此探索了陆内造山过程
The tectonic evolution was discussed mainly on the basis of igneous assemblages. It is suggested that the collision type lithic rocks are the product and mark of ocean closure and land-continent collision, and the muscovite / mica granite is the petrological record of intracontinental subduction. The igneous assemblages dominated by potash basalt series are horizontal shortening Within the boundaries of the orogenic belt mark, Late A-type granite orogenic belt is a sign of the collapse of the orogenic belt. The tectonic evolution and orogenic processes of the Qilian-Qaidam region and the Beishan region have been reconstructed. Discussed the Cenozoic intracontinental orogeny-magmatism and proposed the pairing of the Qinghai-Tibet-Himalaya intracontinental orogenic igneous rocks, thus exploring the intracontinental orogenic processes