|
|||||
|
|
| A 2.8 Ma record of environmental evolution and tectoni events inferred from the Cuoe core in the middle of Tibetan Plateau | |
| 作者姓名： | SHEN Ji Lü Houyuan WANG Sumin CHEN Shiyue YANG Xiangdong WU Yanhong & ZHU Zhaoyu .Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing China .Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China .Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China Correspondence should be addressed to Shen Ji |
| 摘 要： | The uplift of the Tibetan Plateau is the most im-portant event in the Cenozoic Era. It has been provedthat the rising Plateau is of great significance to globalatmospheric circulation and climate change. It has alsoinfluenced the transmission and balance of the globalmatter and energy1—3]. The uplift of the Plateau is un-doubtedly true, but there have long been argumentsabout the process and mode of the Plateau uplift. Didthe Plateau rise as a whole or partly? Did it rise oncefor all or … |
A 2.8 Ma record of environmental evolution and tectoni events inferred from the Cuoe core in the middle of Tibetan Plateau |
|
| Institution: | email: jishen@niglas.ac.cn |
| Abstract: | |
| Keywords: | Tibetan Plateau 2 8 MaBP environmental evolution tectonic events Cuoe Lake |
| 本文献已被 CNKI 等数据库收录！ | |