Pressure evolution and weak low pressure genesis of Shanxi Formation sandstone reservoir in Xinzhao area, northern Ordos Basin
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摘要: 鄂尔多斯盆地北部新召地区上古生界砂岩储层富含天然气且普遍发育异常低压,针对古压力演化以及现今异常低压形成机理认识尚不够深入,制约了致密砂岩气成藏规律的认识和增储上产。本文运用流体包裹体岩相学观察、显微测温和激光拉曼分析技术,综合分析了山西组二段储层中油气充注历史,获取了成藏关键时期的古压力;利用盆地模拟法恢复了古压力演化史,建立了古流体压力演化与油气充注的耦合关系,并进一步探讨了异常低压成因与致密气成藏的成因联系。研究表明:(1)研究区山二段CO2包裹体捕获于距今170~180Ma,此时烃源岩处于中—低成熟阶段,甲烷包裹体捕获于距今138~121Ma的生烃高峰期;(2)山二段储层在早侏罗世开始发育超压,并在早白垩世末规模达到最大,古压力及古压力系数约为50MPa和1.31;(3)由于温度降低、孔隙反弹和气体扩散等因素造成山二段地层压力降低分别约占总地层压力下降幅度的49%,14.5%和36.5%。山二段储层经历了常压—中等超压—常压—低压的演变过程,生烃增压与压力传导是古超压形成的主要原因,温度降低和天然气扩散是山二段异常低压形成的主控因素。 关键词:致密砂岩气;古压力演化;低压成因;山二段;鄂尔多斯盆地Abstract: The Upper Paleozoic sandstone reservoirs in Xinzhao area, northern Ordos Basin are rich in natural gas and generally develop abnormal low pressure. The understanding of paleo-pressure evolution and current subnormal pressure formation mechanism is not very clear, which constraine the understanding of tight sandstone gas accumulation and increase of natural gas reservoir and production. In this paper, the petroleum charging history in the second member of Shanxi Formation was comprehensively analyzed by means of fluid inclusion petrographic observation, micrometry and laser Raman analysis, and the paleo-pressure in the key period of reservoir formation was obtained. The paleo-pressure evolution history was recovered by basin simulation method, and the coupling relationship between paleo-fluid pressure evolution and petroleum charging was established. The relationship between the causes of subnormal pressure and tight gas accumulation is further discussed. The results show that: (1) CO2 was captured in the second member of Shanxi Formation in Xinzhao area from 170 to 180Ma, when the source rock was in the middle to low maturity stage, and the methane inclusion was captured in the peak of hydrocarbon generation from 138 to 121Ma. (2) The overpressure in the second member of Shanxi Formation began to develop in the early Jurassic, and reached the maximum in the end of the Early Cretaceous. The paleo-pressure and paleo-pressure coefficient were about 50MPa and 1.31 respectively. (3) Due to temperature decrease, pore rebound and gas diffusion, the decrease of formation pressure in the second member of Shanxi Formation accounted for 49%, 14.5% and 36.5% of the total formation pressure, respectively. The tight gas reservoir of the second member in Shanxi Formation has undergone the evolution process of normal pressure-medium overpressure-normal pressure and low pressure. Hydrocarbon generation supercharging and pressure conduction are the main reasons for the formation of ancient overpressure. Temperature drop and natural gas diffusion are the main factors for the formation of abnormal low pressure in the second member of Shanxi Formation.
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