中国塔里木盆地塔中地区奥陶系深部碳酸盐岩中气体入侵导致的多相池

IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
AAPG Bulletin Pub Date : 2024-05-01 DOI:10.1306/12212318282
Zhiyao Zhang, Yijie Zhang, Guangyou Zhu, Jianfa Han, Linxian Chi
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引用次数: 0

摘要

揭示具有复杂石油流体相的油气藏的充注历史对于有效勘探和流体预测至关重要。我们利用互补的地球化学数据(如气相色谱、二维气相色谱-飞行时间质谱、特定化合物碳同位素分析和热解模拟)和地质数据分析了中国塔里木盆地塔中地区多相油气藏的油气样品,以更好地了解它们的起源和空间分布。这些数据的整合表明,这些多相池中的石油受到了各种次生地球化学过程的严重影响,包括石油裂解、热化学硫酸盐还原(TSR)和气体侵入。在超过 8500 米(27900 英尺)的深处,寒武纪深层油池中的石油和天然气因超过 170°C (320°F)的高温而发生了石油裂解和 TSR 变化,从而产生了二次产物,包括金刚石类、有机硫化合物 (OSC) 以及经 TSR 变化的富含 H2S 的裂解气。这种寒武纪深层天然气含有菱形物质和有机硫化物,溶解在气相中,通过走向滑动断层向上迁移,侵入奥陶系碳酸盐岩中先前带电的油池,改变了储层流体特征和流体相。因此,由于在原生油中引入了过量的深层气体,形成了凝析油。气体侵入量随着与走向滑动断层距离的增加而减少,从而形成了具有空间分布模式的多相油池。靠近走向滑动断层的油池受气体入侵的影响要大于弱蚀变挥发性油池和距离断层较远的未蚀变油池。断层附近的油池形成的凝析油池显示出 H2S 的富集和 C2-C4 气体组分的碳同位素分馏。这项研究为超深部地层中多相油池的成因机制和分布提供了新的见解,对塔里木盆地深埋奥陶系碳酸盐岩的石油勘探具有巨大的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiphase pools caused by gas invasion in deep Ordovician carbonates from the Tazhong area, Tarim Basin, China
Unraveling the charge histories of pools with complex petroleum fluid phases is crucial for effective exploration and fluid prediction. Oil and gas samples from multiphase pools in the Tazhong area of the Tarim Basin, China, were analyzed using complementary geochemical (e.g., gas chromatography [GC], two-dimensional GC coupled with time-of-flight mass spectrometry, compound-specific carbon isotope analysis, and pyrolysis simulations) and geological data to better understand their origins and spatial distribution. The integration of these data suggests that the petroleum in these multiphase pools was significantly impacted by various secondary geochemical processes, including oil cracking, thermochemical sulfate reduction (TSR), and gas invasion. Oil and gas in deep Cambrian pools were altered by oil cracking and TSR due to high temperatures of more than 170°C (320°F) at depths of more than 8500 m (27,900 ft), leading to the generation of secondary products, including diamondoids, organosulfur compounds (OSCs), and TSR-altered, H2S-rich cracking gases. This deep Cambrian gas, with diamondoids and OSCs, dissolved in the vapor phase, migrated upward through strike-slip faults, and invaded previously charged oil pools in Ordovician carbonates, changing the reservoir fluid characteristics and fluid phases. Thus, condensates were formed due to the introduction of excessive deep gas into the primary oil. The amount of gas invasion decreased with increasing distance from the strike-slip faults, thus forming multiphase pools with a spatial distribution pattern. Oil pools near strike-slip faults are more affected by gas invasion than weakly altered volatile oil pools and unaltered oil pools with greater distances away. The oil pools near the faults form condensate pools that show enrichment of H2S and carbon isotopic fractionation in C2–C4 gas components. This study provides new insights into the causal mechanism and distribution of multiphase pools in superdeep strata and has great potential for petroleum exploration in deeply buried Ordovician carbonates in the Tarim Basin.
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来源期刊
AAPG Bulletin
AAPG Bulletin 工程技术-地球科学综合
CiteScore
6.60
自引率
11.40%
发文量
73
审稿时长
4.8 months
期刊介绍: While the 21st-century AAPG Bulletin has undergone some changes since 1917, enlarging to 8 ½ x 11” size to incorporate more material and being published digitally as well as in print, it continues to adhere to the primary purpose of the organization, which is to advance the science of geology especially as it relates to petroleum, natural gas, other subsurface fluids, and mineral resources. Delivered digitally or in print monthly to each AAPG Member as a part of membership dues, the AAPG Bulletin is one of the most respected, peer-reviewed technical journals in existence, with recent issues containing papers focused on such topics as the Middle East, channel detection, China, permeability, subseismic fault prediction, the U.S., and Africa.
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