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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 1 Electron probe analysis results of minerals in the Lucaogou Formation reservoirs.
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Mineral type | Na2O/% | MgO/% | Al2O3/% | SiO2/% | K2O/% | CaO/% | FeO/% | MnO/% | As2O5/% | SrO/% | CO2/% | Dolomite | 0.194 | 18.873 | 0.051* | 0.118* | 0.022* | 30.681 | 2.488 | 0.251 | 0.484* | 0.198 | 46.640 | Ankerite | 0.083 | 14.393 | 0.036* | BDL | 0.011* | 29.556 | 8.992 | 0.349 | 0.353* | 0.188 | 46.039 | Calcite | 0.099* | 0.490 | 0.034* | 0.050* | 0.016* | 55.313 | 0.665* | 0.160* | | 0.394 | 42.779 | Albite | 11.388 | 0.063* | 19.022 | 67.841 | 0.359 | 0.438* | 0.445 | 0.023* | | 0.421 | | Orthoclase | 0.980 | 0.326 | 17.725 | 67.325 | 12.124 | 0.772 | 0.291 | | | 0.457 | | Microcline | 3.199 | BDL | 18.197 | 66.562 | 11.331 | 0.171 | 0.119 | | | 0.421 | |
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