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王云飞, 王苏民, 薛滨, 吉磊, 吴敬禄, 夏威岚, 潘红玺, 张平中, 陈发虎 (1995)
Sedimentological evidence of the piracy of fossil Zoige Lake by the Yellow River
(1989)
About the fwst author Wang Sumin Born in 1939; graduated from Geography Department of Nanjing University in 1962; now research professor of Nanjing Institute of Geography and Limnology
(1991)
Preliminary study on palaeoclimate and palaeoenvironment of the Qaidam region since three million years ago
(1996)
Timing and height of the Qinghai - Xizang Plateau Uplifting into the cryosphere and its impact on the surrounding area
B. Xue, Su-min Wang, Weilan Xia, Jing-lu Wu, Yunfei Wang, J. Qian, Shouyun Hu, Yanhong Wu, Pingzhong Zhang (1998)
The uplifting and environmental change of Qinghai-Xizang (Tibetan) Plateau in the past 0.9 Ma inferred from core RM of Zoige BasinScience in China Series D: Earth Sciences, 41
(1990)
Palaeoclimatic fluctuation fashion of Qarhan salt lake in Qaidam basin in the past 730,000 years
(1998)
Theuplifting and environmental change of Qinghai-Xizang (Tibetan) plateau in the past 0.9 Ma inferred from core RM
K. Endo, Shun Yan, M. Kanemaki, H. Sohma, G. Mu (1997)
Evolution of Paleoenvironments in Tarim BasinJournal of Geography, 106
(1997)
Palaeoclimate inferred from isotope of lake carbonate of core RM s i n e 140 ka B . P . Science in China ( series D )
(1989)
Lake sedimentation and environment of rift lake in Yunnaa Beijing
(1997)
Evolution of Palaeoenvironments in Tarim Basin - Focussed on the development of Taklimakan Desert
(1998)
Theuplifting and environmental change of Qinghai - Xizang ( Tibetan ) plateau in the past 0 . 9 Ma inferred from core RM of Zoigb Basin
(1997)
Palaeoclimate inferred from isotope of lake carbonate of core RM s i n e 140 ka B.P
(1997)
Evolution of Palaeoenvironments in Tarim Basin-Focussed
Su-min Wang, B. Xue (1997)
Environmental evolution of Zoigê Basin since 900 kaB.P. and comparison study with Loess PlateauScience in China Series D: Earth Sciences, 40
Abstract: Comparative study of long lake records in different regions in China can provide some significant information about the regional differentiation of the environment and Asian monsoon activities. However, intensively studied lacustrine cores with a span of a few hundred thousand years are very rare in China. The available examples are only three long cores from the Zoigê basin in the eastern Qinghai‐Tibet plateau, the Qaidam basin in the northern Qinghai‐Tibet plateau and the Dianchi basin in the Yunnan plateau respectively. The results show that the regional environmental differentiation since the Mid‐Pleistocene involved three stages, i.e. 780–480, 480–160, 160–0 ka B.P. In each of the three stages different regions of China had their own distinctive environmental characteristics, indicating that the uplift of the Qinghai‐Tibet plateau played a major role in the environmental differentiation process.
Acta Geologica Sinica (English Edition) – Wiley
Published: Sep 1, 1998
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