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Factors controlling the development of tight sandstone reservoirs in the Huagang Formation of the central inverted structural belt in Xihu sag, East China Sea Basin
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XU Fanghao,XU Guosheng,LIU Yong,ZHANG Wu,CUI Hengyuan,WANG Yiran
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Table 4 Electronic probe analysis results of quartz secondary overgrowth in central inversion structural belt of the Xihu sag.
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Well | Layer | Depth/m | Composition/% | Na2O | MgO | Al2O3 | SiO2 | K2O | CaO | TiO2 | Cr2O3 | MnO | FeO | NiO | E-3 | H3 | 3 850.4 | 0.001 | 0 | 0.018 | 99.831 | 0.041 | 0.041 | 0 | 0 | 0.015 | 0.052 | 0 | E-3 | H3 | 3 857.9 | 0 | 0.001 | 0.116 | 99.809 | 0.011 | 0 | 0.002 | 0.01 | 0.005 | 0.047 | 0 | E-3 | H3 | 3 857.9 | 0.008 | 0.006 | 0.026 | 99.898 | 0.003 | 0 | 0.019 | 0.004 | 0 | 0.004 | 0.029 | E-3 | H3 | 3 726.6 | 0.028 | 0.008 | 0.006 | 99.795 | 0.07 | 0.028 | 0 | 0 | 0.041 | 0.024 | 0 | E-3 | H3 | 3 795.5 | 0 | 0 | 0.007 | 99.919 | 0.005 | 0.008 | 0.01 | 0.005 | 0.008 | 0.03 | 0.007 | E-3 | H3 | 3 795.5 | 0 | 0 | 0 | 99.793 | 0.02 | 0 | 0.024 | 0 | 0.025 | 0.137 | 0 | E-3 | H4 | 4 023.1 | 0.024 | 0 | 0.095 | 99.853 | 0.026 | 0.002 | 0 | 0 | 0 | 0 | 0 |
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