Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (1): 61-73.doi: 10.13278/j.cnki.jjuese.201701106

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Carbon and Oxygen Isotope Characteristics and Its Significance of Ordovician Carbonates in Yubei Area of Maigaiti Slope

Niu Jun1, Huang Wenhui2, Ding Wenlong2, Jiang Wenlong3, Zhang Yamei2, Qi Lixin4, Yun Lu4, Lü Haitao4   

  1. 1. Faculty of Petroleum, China University of Petroleum-Beijing, Karamay Campus, Karamay 834000, Xinjiang, China;
    2. School of Energy Resource, China University of Geosciences(Beijing), Beijing 100083, China;
    3. Post-Doctoral Research Center, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    4. Exploration and Development Research Institute, Northwest Oilfield Company, Sinopec, Urumqi 830011, China
  • Received:2016-01-12 Online:2017-01-26 Published:2017-01-26
  • Supported by:
    Supported byMajor National Oil and Gas Projects (2011ZX05009-002-203) and Exploration and Development Research Institute, Sinopec Northwest Oilfield Branch Company (KY2011-S-070)

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Abstract: Based on 41 analyzed results of carbon and oxygen isotope, we have discussed the compositions, evolution and geological significance of δ18O and δ13C recorded in the carbonates of Ordovician in Yubei area of Tarim basin, using petrologic method. The result shows that δ13C values range from -2.6‰ to 0.7‰, with average value of -1.0‰; and δ18O values range from -9.4‰ to -3.5‰, with average value of -6.9‰. The values of paleosalinity range from 118.39 to 126.34, with average value of 121.94. The transformation of freshwater in Early Ordovician is strong. The isotopic composition and evolution not only indicate the sedimentary environment, but also show positive correlation with bioproductivity and palaeo-sea level changes:low value of δ13C corresponding to platform shoal of restricted platform environment, high value of δ13C corresponds to interbank sea and platform shoal of open marine platform. Different carbon and oxygen isotopes composition also indicates different diagenetic environments. The δ13C and δ18O value of Yingshan Formation are high negative, which suggest that carbonates experienced strong epigenic karstification. The values of δ13C are low to medium negative and δ18O are high negative in Penglaiba Formation, and saddle dolomite and flint occur in the dolomitite reservoir, indicating that carbonate experienced buried diagenetic environment. The δ13C values in Lianglitage Formation are low positive and δ18O are high negative, which suggest that carbonate experienced buried diagenetic environment.

Key words: carbon and oxygen isotope, depositional environment, carbonates, Ordovician, Maigaiti slope, Tarim basin

CLC Number: 

  • P597
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