中新世以来我国季风-干旱环境演化与青藏高原的生长

- ①中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,西安 710075;
- ②中国地震局地质研究所地震动力学国家重点实验室,北京 100029;
- ③中国科学院地质与地球物理研究所岩石圈演化国家重点实验室,北京 100029;
- ④中国科学院南京地理与湖泊研究所,南京 210008

详细信息

收稿日期: 2006-08-02

刊出日期: 2006-09-25

CHANGES OF THE MONSOON-ARID ENVIRONMENT IN CHINA AND GROWTH OF THE TIBETAN PLATEAU SINCE THE MIOCENE

- ①State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075;
- ②State Key Laboratory Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029;
- ③State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029;
- ④Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008

Received Date: 02 August 2006

Publish Date: 25 September 2006

摘要: 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。
- 季风-干旱环境 /
- 青藏高原生长
Abstract: 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.
- Asian monsoon-arid environment /
-  growth of the Tibetan Plateau

点击查看大图