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Advances in Earth Science  1995, Vol. 10 Issue (3): 254-257    DOI: 10.11867/j.issn.1001-8166.1995.03.0254
Articles     
ODP AND QINGHAI/XIZANG(TIBETAN) PALTEAU
Wang Pinxian
Laboratory of Marine Geology,Tongji University,Shanghai  200092
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Abstract  

    The uplift history of the Tibetan Plateau has been recorded in marine deposits. The two huge deep-sea sediment fans in the Indian Ocean,i: e.,the Bangal Fan and the Indus-River Fan with a total area over 4 million square kilometres,are products of the uplift and erosion of the Himalayas since the middle Tertiary. The enormous sequence of marine deposits in the Yinggehai Basin on the northern shelf of the South China Sea where the Quaternary along reaches 2000m in thickness,is related to the Red River delta and has obviously again resulted from the uplift of the Tibetan Plateau.
    On the other hand, the Plateau's uplift may be the cause or one of the causes of the Cenozoic global cooling and the onset of the Asian monsoon system,as well as the remarkable changes in chemical composition and sedimentation rate of the global ocean.
    All the above discussions are based on discoveries by the DSDP/ODP drillings.Therefore,a research endeavor combining the Tibetan Plateau investigations with the Ocean Drilling Program will be most promisting in breaking through to reveal the mechanism behind the global environmental changes.

Key words:  ODP      Qinghai/Xizang Plateau      Bengal Fan      Global change      Asian monsoon.     
Received:  21 February 1995      Published:  01 June 1995
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Cite this article: 

Wang Pinxian. ODP AND QINGHAI/XIZANG(TIBETAN) PALTEAU. Advances in Earth Science, 1995, 10(3): 254-257.

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http://www.adearth.ac.cn/EN/10.11867/j.issn.1001-8166.1995.03.0254     OR     http://www.adearth.ac.cn/EN/Y1995/V10/I3/254

[1] Johnson M R W. Volume balance of erosional loss and sediment deposition related to Himalayan uplifts. Journal of the Geological Society,London,1994,151(2):217-220.
[2] Stow D A V et al. Sediment facies and processes on the Bengal Fan,Leg 116. Proc Ocean Drilling Program,Scientific Results.1990,116:337-396.
[3] Prell W L, Nittouma N et al. Site 720, Proceedings of the Ocean Drilling Program. Initial Results.1989,117:157-195.
[4] Cochran J R. Himalayan uplift,sea level,and the record of Bengal Fan sedimentation at the ODP Leg 116 sites. Proc Ocean Drilling Program, Scientific Results. 1990,116:397-414.
[5] Klootwijk C T et al. Neogene evolution of the Himalayan-Tibetan region:constraints from ODP Site 758 northern Ninetyeast Ridge;bearing on climate change. Palaeo Palaeo Palaeo,1992,95:95-110.
[6] Weser O E. Sedimentological aspects of strata encountered on Leg 23 in northern Arabian Sea. DSDP Initial Reports,1974,23:503-523.
[7] 汪品先,夏伦煜,王律江,成鑫荣.南海西北陆架的海相更新统下界.地质学报,1991, (2) :176-187.
[8] Davies T A,Hay W W.southam J R and Worsley T R. Estimates of Cenozoic oceanic sedimentation rates. Science, 1977,197:53-55.
[9] Elderfield H. Strontium isotope stratigraphy. Palaeo Palaeo Palaeo,1986, 57:71-90.
[10] Hodell D A. Woodruff F. Variations in the strontium isotopic ratio of seawater during the Miocene:stratigraphic and geochemical implication.Paleoceanography,1994,9(3):405-426.
[11] 同济大学海洋地质系.古海洋学概论.上海:同济大学出版社,1989. 316pp.
[12] Miller K G,Fairbanks R G and Mountain G S. Tertiary oxygen isotope synthesis,sea level history,and continental margin erosion. Paleoceanography,1987,2(1):1-19.
[13] Shackleton N J, Kennett J P. Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation:oxygen and carbon isotopic analyses in DSDP sites 277,279,281. DSDP Initial Rerports. 1975,29:743-755.
[14] Ruddiman W F, Kutzbach J E. Forcing of late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the American west. Jour Geoph Res,1989,94(D15):18379-18391.
[15] Ruddiman W F, Kutzbach J E. Plateau uplift and climate change. Scientific American,1991,March:42-49.
[16] Kutzbach J E,Guetter P J,Ruddiman W F and Prell W L. Sensativity of climate to late Cenozoic uplift in Southern Asia and the American West:numerical experiments. Jour Geoph Res,1989,94(D15):18393-18407.
[17] Wang Pinxian. Neogene stratigraphy and paleoenvironments of China.Palaeo Palaeo Palaeo, 1990,77:315-334.
[18] Wang Pinxian. Progress in Late Cenozoic palacoclimatology in China: a brief review. In: Whyte R O (ed).The Evolution of the East Asian Environment .Hong Kong Univ,1984,1:165-187.

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