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Evolution of abnormally low pressure and its implications for the hydrocarbon system in the southeast uplift zone of Songliao basin, China

机译:松辽盆地东南隆起带异常低压的演化及其对油气系统的影响

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摘要

Underpressured formations are present in the southeast uplift of the Songliao basin, northeast China. At depths between 1540 and 3000 m, the Lower Cretaceous strata in the Shiwu depression of the basin are significantly underpressured at about 50-80% of hydrostatic pressure. Exploration for oil and gas indicates that the hydrocarbon distribution in the depression has unusual characteristics: gas pools occur in the central part of the depression, whereas oil pools occur at the marginal uplift; some gas reservoirs are located at a very shallow depth of 150-450 m. We investigate the mechanism of the abnormal pressures and the characteristics of the hydrocarbon distribution. Numerical modeling indicates that the basin was dominated by overpressure through much of its history and became underpressured only in recent geological time. The earlier overpressurization appears to be essential for the occurrence of the underpressure at the present. The origin of underpressure results primarily from uplift and erosion, as well as reduction of geothermal gradients. Our study also shows that evolution of formation pressure affects not only fluid flow but also hydrocarbon migration and accumulation and gas and oil distribution. The development of underpressure is, therefore, a major factor responsible for habitats of hydrocarbons in the study area.
机译:中国东北的松辽盆地东南隆起存在负压地层。在1540至3000 m的深度处,该盆地十屋凹陷的下白垩统地层在约50-80%的静水压力下明显欠压。对油气的勘探表明,洼地中的碳氢化合物分布具有不同寻常的特征:气藏出现在洼地的中部,而油藏发生在边缘隆起处;一些气藏位于150-450 m的非常浅的深度。我们研究了异常压力的机理和油气分布的特征。数值模拟表明,该盆地在其大部分历史中都以超压为主,仅在最近的地质时期才成为负压。对于目前发生负压而言,较早的过压似乎是必不可少的。负压的起源主要是由于隆升和侵蚀以及地热梯度的减小。我们的研究还表明,地层压力的变化不仅影响流体流动,而且影响烃的运移和聚集以及油气分布。因此,负压的形成是研究区域内碳氢化合物栖息地的主要因素。

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