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Geoscience ›› 2020, Vol. 34 ›› Issue (04): 821-827.DOI: 10.19657/j.geoscience.1000-8527.2020.04.17

• Petroleum Geology • Previous Articles     Next Articles

Strontium Isotope Geochemistry of Ordovician Paleokarst Reservoirs in Huanghua Depression

ZHANG Jinning1,2(), ZHOU Jiansheng2, FU Lixin2, LI Hongjun2, LOU Da2   

  1. 1. China University of Petroleum (Beijing) at Karamay,Karamay,Xinjiang 834000,China
    2. Dagang Oilfield Company, CNPC, Tianjin 300280, China
  • Received:2019-07-05 Revised:2019-09-15 Online:2020-08-31 Published:2020-09-03

Abstract:

To study the strontium (Sr) isotopic characteristics of paleokarst reservoirs, the origin of Sr isotope in Ordovician karst reservoirs in Huanghua depression was discussed via isotopic experiments and comparison with the global Sr isotope background. Isotopic differences between the southern and northern parts of the Huanghua Depression were analyzed. The results show that the 87Sr/86Sr variation range of the Ordovician strata in the Huanghua depression is wider than that of the global Ordovician sedimentation, but their 87Sr/86Sr variation trends are similar. The Ordovician primitive carbonate strata have undergone late paleokarstification and fluid transformation, and the paleo-continental 87Sr-rich fluids were used for various types of karst and filling. The dolomite 87Sr/86Sr values are distinctly higher than those of the limestone in the same horizon, suggesting that the dolomite captures 87Sr more readily than the limestone. Duration of supergene karstification in the northern Huanghua depression is much longer than that in the southern part. The karstification intensity of the former is also higher, and its 87Sr-rich fluid displacement stronger, which probably generates the higher 87Sr/86Sr values in the northern part of Huanghua depression.

Key words: strontium isotope, karstification, reservoir, Huanghua depression, geochemistry, Ordovician

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