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Article Navigation >  Acta Sedimentologica Sinica  > 1986  >  4(4): 87-99

Wang Youxiao, Cheng Xuehui, Wu Yihua, Fan Pu, Jiang Zhusheng. ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI[J]. Acta Sedimentologica Sinica, 1986, 4(4): 87-99.
Citation: Wang Youxiao, Cheng Xuehui, Wu Yihua, Fan Pu, Jiang Zhusheng. ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI[J]. Acta Sedimentologica Sinica, 1986, 4(4): 87-99.
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ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI

  • Lanzhou Institute of Geology, Academia Sinica;

  • Exploration and Development Institute of Xinjiang Petroleum Administration

  • Received Date: 1984-08-13
  • Publish Date: 1986-12-10
  • Erhai is an outpouring freshwater lake of inland fauled type in Yunnan-Guizhou plateau of China, It is 42. 6km long from South to North, and the maximum width is 8.2km. The area is about 250kmz.The maximum depth is 20.7m, Erhai region be- longs to warm climate zone. The lake water is of middle trophic type. It is one of ideal lakes for researching organic geochemistry about recent sediment. Using analyti- cal technique in gas-chromatography, liquid-chromatography, GC/MS and ultraviolet spectrums, etc, Some characteristics in organic geochemistry of the.recent sediment from Erhai have dean obtained as folPowss
  • [1] 中国科学院兰州地质研究所等，1979，青海湖综合考察报告，科学出版社。
    [2] 黄第凡等，1989，陆相有机质演化和成烃机理，石油工业出版社。
    [3] Aizenshatat, Z.，1973, Geochim, et Cosmochim, Acta.，V, 37, P. 559-568
    [4] Limjmbach, G.W.M.，1975, O n the origin of petroleu m, "proceeding of the Ninth World petroleum Congress"，Spi.
    [5] Mackenzie, A.S.et al.，1980, Geochim.et Cosmochim.Acta, V.44, P.1709-1721
    [6] Wakebam S.,G,et al.，1979, Geochim, et Cosmochim, Acta, V. 43, P.1141-1144
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  • Received:  1984-08-13
  • Published:  1986-12-10

ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI

  • Lanzhou Institute of Geology, Academia Sinica;
  • Exploration and Development Institute of Xinjiang Petroleum Administration
  • Received Date: 1984-08-13
  • Publish Date: 1986-12-10

Abstract: Erhai is an outpouring freshwater lake of inland fauled type in Yunnan-Guizhou plateau of China, It is 42. 6km long from South to North, and the maximum width is 8.2km. The area is about 250kmz.The maximum depth is 20.7m, Erhai region be- longs to warm climate zone. The lake water is of middle trophic type. It is one of ideal lakes for researching organic geochemistry about recent sediment. Using analyti- cal technique in gas-chromatography, liquid-chromatography, GC/MS and ultraviolet spectrums, etc, Some characteristics in organic geochemistry of the.recent sediment from Erhai have dean obtained as folPowss

Wang Youxiao, Cheng Xuehui, Wu Yihua, Fan Pu, Jiang Zhusheng. ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI[J]. Acta Sedimentologica Sinica, 1986, 4(4): 87-99.
Citation: Wang Youxiao, Cheng Xuehui, Wu Yihua, Fan Pu, Jiang Zhusheng. ORGANIC GEOCHEMISTRY OF THE RECANT SEDIMEMT FROM ERHAI[J]. Acta Sedimentologica Sinica, 1986, 4(4): 87-99.
shu

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