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板块构造理论中的构造旋回含义与早期经典的强调以不整合为基础的认识不同。对亚洲显生宙特提斯演化和前寒武纪地块及造山历史的分析表明，构造演化是一个均变过程，地质历史早期大陆地壳已显示具有板块构造基本模式特征。板内同造山和造山后变形具有连续性，其中大型走滑断裂的作用相当明显，调整着构造连续演化的统一进程，这在特提斯和中国西北地区表现明显。加里东、海西和阿尔卑斯等经典造山运动或旋回的阶段性特征不复存在。
The meaning of structural gyration in plate tectonic theory is different from that of the early classical emphasis on unconformity. The analysis of the Phanerozoic Tethyan evolution in Asia and the analysis of the Precambrian block and orogenic history shows that the tectonic evolution was a homogeneous process. Early in the geological history, the continental crust has shown the basic pattern of plate tectonics. The same intraplate orogenic or post-orogenic deformation is continuous. Among them, the large-scale strike-slip faults play a quite significant role in adjusting the unitary process of structural continuous evolution, which is evident in Tethys and northwestern China. The classical features of orogenies such as Caledonian, Hercynian and Alpine cease to exist.