Impact of Tethyan domain evolution on the formation of petroleum systems in the Sichuan super basin, SW China

IF 7 Q1 ENERGY & FUELS
Shuyuan SHI , Wei YANG , Gang ZHOU , Hua JIANG , Hao MENG , Saijun WU , Yan ZHANG , Weihua LU , Zhuangzhuang BAI
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Abstract

Based on the “unidirectional break-up and convergence” geodynamic model, this study investigates the impact of the evolution of the Tethyan domain on the formation of petroleum systems in the Sichuan super basin and explores the enrichment pattern of natural gas. The results show that, firstly, the Sichuan Basin and its surrounding areas have experienced two unidirectional rifting-aggregation cycles triggered by the Proto-Tethys Ocean and the Paleo-Tethys Ocean during the Neoproterozoic to Triassic. During Jurassic–Cenozoic, the Sichuan Basin is incorporated in the circum-Tibetan plateau basin-mountain coupled tectonic domain system. The episodic tectonic movements within the plate control the sedimentary infill styles. Second, the evolution of the Tethyan domain, paleoclimatic environment and major geological events controlled the formation and distribution of high-quality source rocks within the basin. The rift valley and intracratonic rift, passive continental margin slope, and intracratonic sags are favorable areas for the development of source rocks. Third, the evolution of the Tethyan domain, supercontinent cycles, global sea level changes, and tectono-climatic events controlled the distribution of carbonate platform and reservoir-caprock combinations. The cratonic platform margins and sub-platform internal high terrains are key areas for finding carbonate high-energy facies belts. Syndepositional paleo-uplifts and surrounding slopes, regional unconformities, and later faults zone are areas where large-scale carbonate reservoirs are distributed. The regional evaporite or shale caprock are beneficial for the large-scale preservation of oil and gas in the basin. Fourth, the spatio-temporal matching relationship of reservoir forming factors influenced by the early tectonic-sedimentary evolution pattern and the degree of later tectonic modification is the key to oil and gas enrichment. Future oil and gas exploration should focus on potential gas systems during the Sinian rift period, Cambrian pre-salt gas systems in the eastern and southern Sichuan, as well as whole oil and gas systems of Permian and Triassic.
中国西南部四川超级盆地特提安岩域演化对石油系统形成的影响
本研究基于 "单向断裂-汇聚 "地球动力学模式,研究了特提斯海域演化对四川超级盆地石油系统形成的影响,并探讨了天然气富集模式。研究结果表明:首先,四川盆地及其周边地区在新元古代至三叠纪经历了由原特提斯洋和古特提斯洋引发的两次单向断裂-聚集循环。在侏罗纪-新生代,四川盆地被纳入环青藏高原盆地-山地耦合构造域系统。板块内部的偶发构造运动控制了沉积的充填方式。其次,哲里木盆地的演化、古气候环境和重大地质事件控制了盆地内优质源岩的形成和分布。裂谷和地壳内裂谷、被动大陆边缘斜坡和地壳内陷是源岩发育的有利区域。第三,特提安岩域的演化、超大陆周期、全球海平面变化以及构造-气候事件控制了碳酸盐岩平台和储层-岩体组合的分布。碎屑岩平台边缘和次平台内部高地形是寻找碳酸盐高能面带的关键区域。同步沉积的古隆起及其周围斜坡、区域性不整合以及后期断层带是大规模碳酸盐岩储层的分布区。区域性蒸发岩或页岩盖层有利于盆地油气的大规模保存。第四,早期构造-沉积演化模式与后期构造改造程度影响成藏因素的时空匹配关系是油气富集的关键。未来油气勘探应重点关注新元古代裂谷期潜在气系、川东和川南寒武系前盐气系以及二叠系和三叠系整体油气系统。
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CiteScore
11.50
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