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Acid-base alternation diagenesis and its influence on shale reservoirs in the Permian Lucaogou Formation, Jimusar Sag, Junggar Basin, NW China
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WANG Jian,ZHOU Lu,LIU Jin,ZHANG Xinji,ZHANG Fan,ZHANG Baozhen
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Table 3 XRD analysis results of clay minerals in the Lucaogou Formation reservoirs.
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Well | Depth/m | Montmorillonite/% | Illite/mosnt- morillonite/% | Illite/ % | Kaolinite/ % | Chlorite/ % | Chlorite/mont- morillonite/% | Ratio of the illite/ montmorillonite/% | Ratio of chlorite/ montmorillonite/% | Ji 174 | 3128.10 | | 44 | | | 56 | | 70 | | Ji 174 | 3141.04 | | | 3 | | 11 | 86 | | 40 | Ji 174 | 3197.79 | 100 | | | | | | 100 | | Ji 174 | 3206.44 | 94 | | | | 6 | | 100 | | Ji 174 | 3267.19 | | 69 | | | | 31 | 90 | 30 | Ji 174 | 3296.61 | | 100 | | | | | 95 | | Ji 174 | 3314.46 | | 95 | 5 | | | | 80 | | Ji 174 | 3378.36 | | | 6 | | 18 | 76 | | 20 | Ji 174 | 3392.77 | | | 28 | | 16 | 56 | | 30 | Ji 251 | 3601.06 | | 85 | 15 | | | | 20 | | Ji 251 | 3619.61 | | 11 | 54 | | 28 | 7 | 20 | 30 | Ji 251 | 3629.18 | | | 12 | | | 88 | | 30 | Ji 251 | 3631.99 | | 47 | 29 | | 24 | | 55 | | Ji 251 | 3632.35 | | 2 | 35 | | 34 | 29 | 20 | 40 | Ji 251 | 3633.07 | | | 37 | | 48 | 15 | | 40 | Ji 251 | 3744.72 | | 100 | | | | | 60 | | Ji 251 | 3770.33 | | 100 | | | | | 60 | | Ji 251 | 3878.49 | | 83 | 8 | | 9 | | 95 | | Ji 303 | 2592.00 | | 52 | 29 | 6 | 13 | | 75 | | Ji 303 | 2592.77 | | 63 | 19 | 7 | 11 | | 65 | | Ji 303 | 2600.32 | | 64 | 20 | 3 | 13 | | 65 | | Ji 305 | 3576.78 | | 79 | 13 | | 8 | | 90 | | Ji 34 | 3684.59 | | | | 10 | 90 | | | | Ji 34 | 3781.22 | | 60 | 27 | 4 | 9 | | 20 | | Ji 34 | 3811.43 | | 11 | 61 | 6 | 22 | | 20 | | Ji 34 | 3811.70 | | 26 | 40 | 7 | 27 | | 40 | | Ji 34 | 3812.34 | | 85 | 11 | 2 | 2 | | 85 | | Ji 34 | 3813.00 | | 31 | 53 | 7 | 9 | | 80 | | Ji 34 | 3815.65 | | 91 | 1 | 2 | 6 | | 40 | | Ji 38 | 2785.22 | | 53 | 15 | | 32 | | 90 | | Ji 38 | 2809.43 | | 60 | 14 | | 26 | | 45 | | Ji 43 | 2924.27 | | | 10 | | | 90 | | 30 | Ji 43 | 2948.26 | | 97 | 3 | | | | 90 | | Ji 43 | 2961.93 | | 3 | 6 | | 11 | 80 | 20 | 40 |
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