Origin and Evolution Process of Overpressure in the Shahezi Formation of Xujiaweizi Fault Depression in the Northern Songliao Basin, NE China

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Chengju ZHANG, Zhenxue JIANG, Jiamin LU, Lidong SHI, Zhongyu BI, Lidong SUN, Liang YANG, Xiaomei LI, Jiajun LIU, Huan MIAO
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Abstract

It is of great significance for deep oil and gas exploration to understand the origin and evolution behind overpressure. Overpressure occurs in the deep Shahezi Formation of Xujiaweizi fault depression. However, due to limited degree of exploration, there are some problems in the study area, such as unclear understanding of the origin of overpressure and the vague investigation of overpressure evolution. To clarify the impact of overpressure on oil and gas migration and accumulation in the study area, this study focuses on the research of the origin and evolution of overpressure in the Shahezi Formation of the study area, utilizing single well logging parameters and combining methods such as microthermometry of fluid inclusions, laser Raman spectrum, and basin simulation. The results show that the overpressure of the Shahezi Formation in Xujiaweizi fault depression is primarily generated by hydrocarbon generation pressurization, and the evolution of overpressure is closely related to hydrocarbon generation. The development of overpressure can be divided into two evolutionary stages: early hydrocarbon generation pressurization and late uplift release, with slight variations in different regions. Tight glutenite gas reservoirs in the Shahezi Formation are characterized by continuous charging. The overall charging period ranges from the late Denglouku to the early Mingshui (110‐67 Ma ago). There is an obvious paleo‐overpressure during the gas reservoir formation period. The gas generation period of source rocks occurred approximately 125‐60 Ma ago, and the main gas generation period (112‐67 Ma ago) highly coincides with the period of natural gas charging. The anomalously high pressure during the accumulation period is considered the significant driving force for natural gas charging. In addition, the sustained effect of overpressure provides better conditions for the preservation of tight gas reservoirs within the source. The results of the study are of guiding significance for the in‐depth exploration and development of deep tight sandstone gas in the Shahezi Formation of Xujiaweizi fault depression.
中国东北松辽盆地北部徐家围子断陷沙河子地层超压成因及演化过程
了解超压的起源和演化过程对深层油气勘探具有重要意义。徐家围子断陷深部沙河子地层存在超压现象。但由于勘探程度有限,研究区存在超压成因认识不清、超压演化研究模糊等问题。为明确超压对研究区油气运移和聚集的影响,本研究利用单井测井参数,结合流体包裹体微测温、激光拉曼光谱、盆地模拟等方法,重点研究了研究区沙河子地层超压的成因和演化。结果表明,徐家围子断陷沙河子地层的超压主要由油气生成加压产生,超压的演化与油气生成密切相关。超压的发展可分为两个演化阶段:早期油气生成加压和晚期隆起释放,不同地区略有差异。沙河子地层的致密谷甾醇气藏具有持续充注的特点。整体充注期为登楼晚期至明水早期(距今110-67Ma)。气藏形成期存在明显的古超压现象。气源岩的成气期约在距今125-60Ma,主成气期(距今112-67Ma)与天然气充注期高度重合。积聚期的异常高压被认为是天然气充注的重要驱动力。此外,持续的超高压效应也为气源内部致密气藏的保存提供了更好的条件。研究结果对徐家围子断陷沙河子地层深部致密砂岩气的深入勘探开发具有指导意义。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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