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    Volume 38 Issue 4
    Jul.  2013
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    Article Navigation >  Earth Science  > 2013  >  38(4): 819-831
    GAO Da, LIN Chang-song, YANG Hai-jun, ZUO Fan-fan, CAI Zhen-zhong, LIU Jing-yan, ZHANG Li-juan, LI Hong, 2013. Microfacies of Late Ordovician Lianglitage Formation and Their Control on Favorable Reservoir in Tazhong Area. Earth Science, 38(4): 819-831. doi: 10.3799/dqkx.2013.080
    Citation: GAO Da, LIN Chang-song, YANG Hai-jun, ZUO Fan-fan, CAI Zhen-zhong, LIU Jing-yan, ZHANG Li-juan, LI Hong, 2013. Microfacies of Late Ordovician Lianglitage Formation and Their Control on Favorable Reservoir in Tazhong Area. Earth Science, 38(4): 819-831. doi: 10.3799/dqkx.2013.080
    shu

    Microfacies of Late Ordovician Lianglitage Formation and Their Control on Favorable Reservoir in Tazhong Area

    doi: 10.3799/dqkx.2013.080
    • 1.

      School of Energy Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      School of Ocean Sciences, China University of Geosciences, Beijing 100083, China

    • 3.

      Research Institute of Petroleum Exploration and Production, Tarim Oilfield Company, PetroChina, Korla 841000, China

    • Received Date: 2013-01-28
    • Publish Date: 2013-07-01
      Abstract
    • The Lianglitage Formation has been of great scientific interest for being the main reservoir for oil and gas in Tazhong area, Tarim basin. However, researches on depositional microfacies and their controls on reservoir quality are inadequate. Based on cores, thin-sections and well-logging data, detailed microfacies analysis, high-resolution sequences and controlling factors on favorable reservoir are studied in this paper. 9 microfacies (Mf1-Mf9) are recognized in carbonate platform and 3 microfacies associations(MA1-MA3) are established, which are interpreted as platform margin reef and sand bank, platform margin-interior sand bank, and platform interior peri-tidal types respectively. One or more microfacies associations can be developed within a fourth order sequence which is constrained by subordinated flood surface. Depositional model for HST of SQ2 is constructed, based on high-resolution sequences and microfacies analysis and their correlation between wells. The high energy microfacies are the primitive material for favorable reservoir, because they might have been more probably to be dissolved by meteoric water during penecontemporaneous diagenetic progress, and also more easily to be fractured. The reservoir quality of low energy microfacies could have been improved if tectonic fractures, burial dissolution and/or karstification developed.

       

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