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Research on thin reservoir prediction method in the coal seam distribution area |
Xue YANG1, Jia-Xue PEI1, Shao-Yong HE1, Xue-Feng JIANG1, Tian-Shou XIE2, Jian-Jun GAO1 |
1. Exploration and Development Research Institute of Liaohe Oil Field CNPC, Panjin 124010, China 2. Exploration and Development Research Institute of Xinjiang Oil Field CNPC, Keramay 834000, China |
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Abstract There are multiple combinations of sandstone and mudstone interbeds and also plenty of coal seams in the middle-shallow strata of Mahu sag's slope zone, due to the slow slope background and shallow lake environment of water oscillation since Jurassic. In addition, the lithologic reservoir can be found in the zone, but the shielding effect of coal seam makes it impossible to predict the reservoir, due to the unclear response of the thin interbed from seismic and acoustic logs. Therefore, the wave impedance inversion cannot distinguish sandstone from mudstone clearly. In view of such a situation, the technique of Pseudo-acoustic curve reconstruction was used in this study. By analyzing multiple well logs, the density and neutron curves, which can weaken the influence of coal seam and reflect the characteristics of sandstone and mudstone interbeds, were selected to rebuild pseudo-acoustic curves and then perform inversion with the rebuilt curves, thus improving greatly the accuracy of reservoir prediction.
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Received: 14 August 2019
Published: 22 April 2020
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Regional structure outline map of Mahu sag
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岩 性 | 中 子 | 密度 /(g·cm-3) | 时差 /(μs·ft-1) | 纵波速度 /(m·s-1) | 纵波阻抗 /(g·cm-3·m·s-1) | 煤 层 | 0.30~0.64 | 1.36~2.32 | 90~125 | 2400~3300 | 3200~7600 | 泥 岩 | 0.27~0.51 | 1.67~2.63 | 75~88 | 3500~4100 | 5800~10800 | 储层砂岩 | 0.19~0.42 | 1.58~2.46 | 71~77 | 3900~4300 | 7200~10500 | 致密砂岩 | 0.16~0.33 | 2.45~2.62 | 59~68 | 4500~5200 | 11000~13600 |
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Statistical data of petro-physical parameters and logging characters of different types rocks
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Well M612 comprehensive log-curves
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Comparison of synthetic seismogram by original sonic(a) and Pseudo sonic(b)
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Comparison of original sonic inversion section(a) and Pseudo sonic inversion section(b)
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