LIU Jia
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The fifth member of the Ordovician Majiagou Formation (Ma 5 Member) in Daniudi gasfield is standing in regression. Vertically, it is divided into 10 submembers (Ma 51 to Ma 510), among which Ma 51+2 is still in relative regression. Numerous dissolved pores, vugs and fractures induced from fresh water leaching and karstification are extended into Ma 51+2 where gray dolomite is dominantly developed with a little limestone to accumulate hydrocarbon. Therefore, cores, well- and mud-logging data from over 580 wells drilling through the target were analyzed to predict geological sweetspots of Ma 51+2 in this field. And that there developed 4 types of sedimentary microfacies, including calcareous dolomite flat, dolomite flat, dolomitic limestone flat, and argillaceous dolomite flat, was pointed out. Furthermore, combined with paleogeomorphological natures, the thickness distribution of Ma 51+2 reservoirs on the plane was characterized. By referring to production data of gas wells, the extension of quality reservoirs was predicted, and the sweetspots were delineated. Results show that (i) 7 episodes of sedimentary cycle are developed vertically in Ma 51+2 where shale content increases from below, meaning the decreasing trend of waterbody depth and salinity while this content decreases from north to south on profile, implying the increasing trend of waterbody depth and salinity; and (ii) Ma 51+2 reservoirs overall get thicker to the west, and their thickness varies greatly along north to south, with the maximum thickness difference of 24 m, but gently along east to west, with the maximum difference of 8 m. Six geomorphological units are identified, i.e., karst platform mound, monadnock, slope, highland, low-lying land and trough, and the reservoirs are mainly located in the first two units. In conclusion, the quality reservoirs are mainly deposited in both calcareous dolomite flat and dolomite flat. Rich in dolomite extended from northeast to southwest, the residual reservoirs are thick. This thickness often exceeds 4 m in both platform mound and monadnock, and that from 2 to 6 m in slope. Additionally, three sweetspot zones are selected on the basis of predominant microfacies, lithofacies and paleogeomorphological units. With the porosity exceeding 2.5%, the quality reservoirs are over 4 m in thickness. Imaging logging presents that fractures, dissolved pores and vugs are well developed, indicating better physical properties. Both gas saturation and total hydrocarbon content are over 15% and 20%, respectively. The testified cumulative production is more than 2000×104 m3.