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| A 2.8 Ma record of environmental evolution and tectoni events inferred from the Cuoe core in the middle of Tibetan Plateau | |
| 引用本文： | SHEN Ji1,Lü Houyuan2,WANG Sumin1,CHEN Shiyue1,YANG Xiangdong1,WU Yanhong1 & ZHU Zhaoyu3 1.Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008,China,2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China,3.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China Correspondence should be addressed to Shen Ji(email: jishen@niglas.ac.cn). A 2.8 Ma record of environmental evolution and tectoni events inferred from the Cuoe core in the middle of Tibetan Plateau[J]. 中国科学D辑(英文版), 2004, 0(11) |
| 作者姓名： | SHEN Ji1 Lü Houyuan2 WANG Sumin1 CHEN Shiyue1 YANG Xiangdong1 WU Yanhong1 & ZHU Zhaoyu3 1.Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing 210008 China 2.Institute of Geology and Geophysics Chinese Academy of Sciences Beijing 100029 China 3.Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou 510640 China Correspondence should be addressed to Shen Ji(email: jishen@niglas.ac.cn) |
| 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 energy[1—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 |
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| Affiliation: | email: jishen@niglas.ac.cn |
| Abstract: | |
| Keywords: | Tibetan Plateau 2.8 MaBP environmental evolution tectonic events Cuoe Lake. |
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