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板块构造学说是高度成功的地球科学理论。大洋岩石圈与大陆岩石圈之间的多岛弧盆系构造域是板块构造登陆的入门向导。青藏高原大地构造研究实践表明,青藏高原是板块构造登陆的研究基地。众多蛇绿岩带、混杂岩带和火山岩浆弧带等的识别,支持洋陆转换多岛弧盆系构造模式,可用来解释特提斯和亚洲大陆的形成和演化。
Plate tectonics is a highly successful geoscience theory. The multi-island arc basin tectonic domain between the oceanic lithosphere and the continental lithosphere is an introductory guide to plate tectonics. The research on the tectonics of the Qinghai-Tibet Plateau shows that the Qinghai-Tibet Plateau is the research base for plate tectonic logging. The identification of numerous ophiolite zones, melange zones and volcanic magma arcs supports the conversion of multi-island arc basins to oceanic continents and can be used to explain the formation and evolution of the Tethyan and Asian continents.