Enrichment model and major controlling factors of below-source tight oil in Lower Cretaceous Fuyu reservoirs in northern Songliao Basin, NE China

IF 7 Q1 ENERGY & FUELS
Xiaojun WANG , Xuefeng BAI , Junhui LI , Zhijun JIN , Guiwen WANG , Fangju CHEN , Qiang ZHENG , Yanping HOU , Qingjie YANG , Jie LI , Junwen LI , Yu CAI
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Abstract

Based on the geochemical, seismic, logging and drilling data, the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics, the tight oil enrichment model and its major controlling factors. First, the Quantou Formation is overlaid by high-quality source rocks of the Upper Cretaceous Qingshankou Formation, with the development of nose structure around sag and the broad and continuous distribution of sand bodies. The reservoirs are tight on the whole. Second, the configuration of multiple elements, such as high-quality source rocks, reservoir rocks, fault, overpressure and structure, controls the tight oil enrichment in the Fuyu reservoirs. The source-reservoir combination controls the tight oil distribution pattern. The pressure difference between source and reservoir drives the charging of tight oil. The fault-sandbody transport system determines the migration and accumulation of oil and gas. The positive structure is the favorable place for tight oil enrichment, and the fault-horst zone is the key part of syncline area for tight oil exploration. Third, based on the source-reservoir relationship, transport mode, accumulation dynamics and other elements, three tight oil enrichment models are recognized in the Fuyu reservoirs: (1) vertical or lateral migration of hydrocarbon from source rocks to adjacent reservoir rocks, that is, driven by overpressure, hydrocarbon generated is migrated vertically or laterally to and accumulates in the adjacent reservoir rocks; (2) transport of hydrocarbon through faults between separated source and reservoirs, that is, driven by overpressure, hydrocarbon migrates downward through faults to the sandbodies that are separated from the source rocks; and (3) migration of hydrocarbon through faults and sandbodies between separated source and reservoirs, that is, driven by overpressure, hydrocarbon migrates downwards through faults to the reservoir rocks that are separated from the source rocks, and then migrates laterally through sandbodies. Fourth, the differences in oil source conditions, charging drive, fault distribution, sandbody and reservoir physical properties cause the differential enrichment of tight oil in the Fuyu reservoirs. Comprehensive analysis suggests that the Fuyu reservoir in the Qijia–Gulong Sag has good conditions for tight oil enrichment and has been less explored, and it is an important new zone for tight oil exploration in the future.

中国东北松辽盆地北部下白垩统扶余油藏致密油富集模型及主要控制因素
根据地球化学、地震、测井和钻井资料,从地质特征、致密油富集模式及其主要控制因素等方面,对松辽盆地北部下白垩统泉头地层富余油藏进行了系统研究。首先,泉头地层为上白垩统青山口地层优质源岩所覆盖,围陷鼻状构造发育,砂体分布广且连续。储层整体致密。其次,优质源岩、储层岩、断层、超压和构造等多元素的配置控制着扶余油藏的致密油富集。源-储层组合控制致密油分布模式。油源与储层之间的压力差推动致密油的充注。断层-砂体运移系统决定了油气的迁移和聚集。正断层构造是致密油富集的有利场所,断层-地角带是同步带致密油勘探的关键部位。第三,根据源-储层关系、运移方式、富集动态等要素,确认了扶余油藏致密油富集的三种模式:(1)烃类从源岩垂直或横向迁移至相邻储层岩,即在超压驱动下,生成的烃类垂直或横向迁移至相邻储层岩并聚集;(2)烃类通过断层在分离的源岩和储层之间运移,即在超压驱动下,烃类通过断层向下运移至与源岩分离的砂体;(3) 油气通过断层和砂体在分离的源岩和储层之间迁移,即在超压的驱动下,油气通过断层向下迁移到与源岩分离的储层岩石,然后通过砂体横向迁移。第四,油源条件、充注驱动、断层分布、砂体和储层物性的差异,导致扶余油藏致密油富集程度不同。综合分析表明,齐家-古浪下陷扶余油藏致密油富集条件好,勘探程度低,是未来致密油勘探的重要新区。
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CiteScore
11.50
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473
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