鄂尔多斯盆地中东部延长组异常低压的形成、发展及其影响因素

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Lijuan HE, Qiang YU, Zhanli REN, Rongxi LI, Xianghe LEI, Xianyao SUN, Qike YANG, Tianzi WANG, Ruize YUAN
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引用次数: 0

摘要

现今的压力格局是古压力演化的最终结果,因此了解整个地质历史中应力的变化对油气聚集具有重要意义。本文采用裂变径迹法重建了延长组砂岩样品的冷却历史。鄂尔多斯盆地中东部及延长组低压异常成因分析。进行了分析。马克斯。利用Petromod 1D软件,重建了福潭1井地层埋深压力,模拟了地层压力演化。核裂变径迹数据和Petromod 1D模拟结果表明,延长组的核裂变径迹数据表明:达到了最大值。古压力为30.92 MPa,约为100 Ma。晚白垩世以来,研究区地层压力演化可分为两个阶段。100 ~ 20 Ma,地层缓慢抬升,压力逐渐降低。中新世(约20 Ma)以来,压力迅速下降至目前的约6.92 MPa。在上述研究结果的基础上,定量计算了孔隙回弹和温度降低对地层压力的影响。结果表明:在第一阶段,孔隙回弹和冷却导致的压力降低分别为3.86 MPa和3.49 MPa,分别降低了12.48%和11.28%;在第二阶段,孔隙回弹和冷却导致的压力降低分别为6.32 MPa和9.60 MPa,分别降低了约20.43%和31.04%。延长组低压的形成。盆地中东部主要受地层隆升后侵蚀引起的孔隙回弹和温度降低控制。温度的降低对低压油藏的形成过程起着决定性的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Formation and Development of Abnormal Low Pressure in the Yanchang Formation of the Central–Eastern Ordos Basin and its Influencing Factors

Formation and Development of Abnormal Low Pressure in the Yanchang Formation of the Central–Eastern Ordos Basin and its Influencing Factors

The present-day pressure pattern is the ultimate result of the evolution of paleo-pressure, so understanding the variation of stress throughout geological history is of great significance for oil and gas accumulation. In this study, the fission track method was used to reconstruct the cooling history of sandstone samples from the Yanchang Fm. in the central–eastern Ordos Basin and the cause of the low-pressure anomaly in the Yanchang Fm. was analyzed. The max. burial depth pressure was reconstructed and the pressure evolution of the formation in the Futan 1 well was simulated, using Petromod 1D. The fission track data and Petromod 1D simulation results indicate that the Yanchang Fm. reached its max. burial depth and experienced a high paleo-pressure of 30.92 MPa at around 100 Ma. Since the Late Cretaceous, the formation pressure evolution in the study area can be divided into two stages. From 100 to 20 Ma, the formation slowly uplifted, with the pressure gradually decreasing. Since the Miocene (about 20 Ma), the pressure rapidly decreased to the current pressure of approximately 6.92 MPa. Based on the above research results, the influence of pore rebound and temperature decrease on formation pressure was quantitatively calculated. The results show that during the first stage, the pressure reduction caused by pore rebound and cooling was 3.86 MPa and 3.49 MPa, respectively, with a decrease of about 12.48% and 11.28%. During the second stage, the pressure reduction caused by pore rebound and cooling was 6.32 MPa and 9.60 MPa, respectively, with a decrease of about 20.43% and 31.04%. The formation of low pressure in the Yanchang Fm. in the central and eastern basin is mainly controlled by pore rebound and temperature reduction, caused by erosion after stratigraphic uplift. The decrease in temperature plays a decisive role in determining the formation process of the low-pressure oil reservoir.

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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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