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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 1 Rock clastic composition of the Huagang Formation in the north-central part of the central inversion tectonic belt in the Xihu sag.
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Sublayer | Depth/m | Q1/% | F1/% | R1/% | Q1/(F1+R1) | F1/R1 | Number of samples | H3 | 3 245 | 63.5 | 16.8 | 19.7 | 1.74 | 0.86 | 541 | H4 | 3 459 | 64.8 | 16.6 | 18.6 | 1.84 | 0.89 | 414 | H5 | 3 615 | 64.9 | 16.4 | 18.7 | 1.85 | 0.87 | 110 | H6 | 3 874 | 64.0 | 16.7 | 19.3 | 1.77 | 0.87 | 122 | H7 | 4 334 | 65.3 | 16.2 | 18.6 | 1.88 | 0.87 | 87 | Average | 3 705 | 64.5 | 16.5 | 19.0 | 1.80 | 0.87 | 1274* |
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