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Orderly coexistence and accumulation models of conventional and unconventional hydrocarbons in Lower Permian Fengcheng Formation, Mahu sag, Junggar Basin
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ZHI Dongming,TANG Yong,HE Wenjun,GUO Xuguang,ZHENG Menglin,HUANG Liliang
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Table 1 Geochemical parameters of hydrocarbon source rocks of different lithologies from the Fengcheng Formation of the Mahu sag, Junggar Basin.
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Lithology | TOC/% | S1/(mg·g-1) | (S1+S2)/(mg·g-1) | HI/(mg·g-1) | Tmax/°C | Value range | Proportion of values larger than 0.6 | Value range | Proportion of values larger than 1 | Value range | Proportion of values larger than 2 | Value range | Proportion of values larger than 250 | Mudstone | Dolomitic mudstone, silty mudstone, tuffaceous mudstone | 0.03-2.79 1.04(157) | 71.34% | 0.01-9.35 1.42(154) | 51.30% | 0.01-25.29 5.18(157) | 71.34% | 2.67-981.82 290.97(157) | 52.23% | 359-489 426(157) | Dolomite | Silty dolomite, argillaceous dolomite, tuffaceous dolomite | 0.12-3.11 0.99(48) | 68.75% | 0.01-3.79 0.77(47) | 25.53% | 0.01-23.58 4.82(48) | 68.75% | 3.33-817.05 331.61(48) | 66.67% | 311-579 430(48) | Tuff | Silty tuff, dolomitic tuff, tuffite | 0.25-3.58 1.02(31) | 64.52% | 0.01-3.62 0.71(31) | 29.03% | 0.01-24.05 4.07(31) | 64.52% | 10.34-688.46 331.61(30) | 66.67% | 407-454 434(31) | Siltstone | Dolomitic siltstone, tuffaceous siltstone, argillaceous siltstone | 0.20-4.08 1.96(31) | 96.77% | 0.05-3.93 2.45(31) | 96.77% | 0.27-14.13 8.23(31) | 96.77% | 110.00-490.40 310.75(31) | 74.19% | 411.0-430.0 421.7(31) |
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