根据中国北方地质、生物和构造记录与南海及全球记录的对比研究,讨论了中国中新世以来季风-干旱环境与青藏高原阶段性生长耦合演化的关系。研究认为,在研究季风环境的同时,应加强我国季风-干旱环境整体系统变迁及其动力学的研究。
On the basis of the comparison of the paleorecords among the North China, the South China Sea and the globe, we have discussed the coupling relationship between changes of the monsoon-arid environment and phased growth of the Tibetan Plateau since the Miocene in China. The authors pointed out that the study of the evolution and dynamics of the monsoon-arid environment system should be paid attention to, while the study of the monsoon environment is underway simultaneously.