Li Jijun;Fang Xiaomin;Pan Baotian,Late Cenozoic intensive uplift of Qinghai-Xizang Plateau and its impacts on environments in surrounding area,Quaternary Sciences,2001(05).
[4]
Cui Zhijiu;Wu Yongqiu;Liu Gengnian,On Kunlun-Yellow River tectonic movement,Scinece in China (Series D)? ,1998, 41(06).
Shi Yafeng;Li Jijun;Li Bingyuan,The late Cenozic uplift and environmental changes of the Qinghai--Xizang Plateau,广州:广东科技出版社,1998.
[10]
Qi Wen;Zheng Mianping.Precipitation fluctuation since 30.0 ka BP at Chabyer Cuka,western Tibet[J].Acta Geoscientia Sinica,2005(01)
[11]
Molnar P T;England P,Late Cenozoic uplift of mountain ranges and global climate change:chicken or egg,NATURE,1990.
[12]
齐文;郑绵平.西藏扎布耶盐湖30.0 ka BP以来水位与古降水量变化[J].地球学报,2005(01)
[13]
Chen Shiyue;Jin Zhangdong;Wang Sumin.Late Cenozoic chemical weathering and environmental changes recorded in the Co Ngoin sediments,central Qinghai-Tibet Plateau[J].Acta Geologica Sinica(English Edition),2005(03)
[14]
Zhao Xitao;Zhu Dagang;Wu Zhonghai.The development of Nam Co lake in Tibet since late Pleistocene[J].Acta Geoscientia Sinica,2002(04)
[15]
Wu Yanhong;Wang Sumin;Xia Weilan,Environmental variation in central Tibetan Plateau in the last 200 years,Science in China Ser D,2001(zk).
[16]
Wu Jinglu;Wang Sumin,Environmental characteristics showed by δ18O and δ13C of authicarbonate in core RM from Zoige basin,Marine Geology & Quaternary Geology,1997(04).
[17]
Wang Sumin;Wu Xihao;Zhang Zhenke.Sedimentary records of environmental evolution in the Sanmen Lake Basin and the Yellow River running through the Sanmenxia Gorge eastward into the sea[J].Science in China Ser D,2002(07)doi:10.1360/02yd9061
[18]
Wang Sumin;Li Jianren,Lacustrine sediments-an indicator of historical climatic variations--The case of Qinghai Lake and Daihai Lake,Chinese Science Bulletin,1991(16).
[19]
Raymo M E;Ruddiman W F;Backman J,Late Pliocene variation in Northern Himisphere ice sheet and north Atlantic deep water circulation,PALEOCEANOGRAPHY,1989(04).
[20]
Lü Houyuan;Wang Sumin;Wu Naiqing,A new pollen record of the last 2.8 Ma from the Co Ngoin,central Tibetan Plateau,Science in China Ser D,2001(zk).