China Petroleum Exploration ›› 2015, Vol. 20 ›› Issue (3): 30-37.

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Prediction of Dolomite Reservoir Distribution on Top of Triassic Leikoupo Formation in Chuanxi Depression

NingMeng1,LiuShu2,GongWenping1   

  1. 1School of Geosciences of Yangtze University
    2Exploration and Development Research Institute of Sinopec Southwest Oil and Gas Company
  • Online:2015-05-15 Published:2015-05-22
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Abstract:

The weathering crust reservoir developed on the top of Triassic Leikoupo Formation in Chuanxi depression. Recently, a high-yield industrial gas flow was acquired from Well PZ1 drilled at this weathering crust, indicating a great oil and gas potential of Leikoupo Formation, but the failure of Well TS1 also shows complexity of the gas reservoir. The grained dolomite with dissolved pores is the main reservoir in the 4th member of Leikoupo Formation in Chuanxi depression. Based on the dolomite flat, the high-quality reservoir came under dolomite diagenetic transformation in the later period. However, thanks to interferences of faults and gypsum in Leikoupo Formation, it is difficult to predict reservoirs by means of seismic reflection structure. The study indicates that the top of Leikoupo Formation in Chuanxi depression is characterized with unique fault facies. Two small arc-shaped fault belts developed in the depression, which are dolomite with strong fault deformation facies. The complete anticline with the faults undeveloped was behind the fault belt and in the form of dolomite with weak fault deformation facies. The eastern slope of the depression is crumpled gypsum facies. Based on the unique characteristics of fault and geo-mechanical principles, the two small arc-shaped fault belts are predicted as rigid formations with the single layers being thin and dolomite flat marginal facies. The layers of reservoir are relatively thin but with development of fractures. The complete block behind the fault belts is the rigid formation with the single layers being thick and dolomite flat central facies. Thickness of the reservoir is large. The crumpled zone east of the small fault belts is gypsum development zone.

 

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