Microscopic mechanisms of intrasource micro-migration and enrichment of lacustrine shale oil: A case study of Chang73 submember of Triassic Yanchang Formation, Ordos Basin, NW China

IF 10.7 Q1 ENERGY & FUELS
Petroleum Exploration and Development Pub Date : 2025-10-01 Epub Date: 2025-10-30 DOI:10.1016/S1876-3804(25)60639-2
Yingzhu WANG , Yuting HOU , Jijin YANG
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引用次数: 0

Abstract

To clarify the mechanism of differential enrichment of intrasource shale oil, taking the third of seventh member of the Triassic Yanchang Formation (Chang73 submember for short) in the Ordos Basin, NW China as an example, we integrated high-resolution scanning electron microscopy (SEM), optical microscopy, laser Raman spectroscopy, rock pyrolysis, and organic solvent extraction experiments to identify solid bitumen of varying origins, obtain direct evidence of intrasource micro-migration of shale oil, and establish the coupling between the shale nano/micro-fabric and the oil generation, migration and accumulation. The Chang73 shale with rich alginite in laminae has the highest hydrocarbon generation potential but a low thermal transformation ratio. Frequent alternations of micron-scale argillaceous-felsic laminae enhance the hydrocarbon expulsion efficiency, yielding consistent aromaticity between in-situ and migrated solid bitumen. Mudstone laminae rich in terrestrial organic matter (OM) and clay minerals exhibit lower hydrocarbon generation threshold but stronger hydrocarbon retention capacity, with a certain amount of light oil/bitumen preserved to differentiate the chemical structure of in-situ versus migrated bitumen. Tuffaceous and sandy laminae contain abundant felsic minerals and migrated bitumen. Tuffaceous laminae develop high-angle microfractures under shale overpressure, facilitating oil charging into rigid mineral intergranular pores of sandy laminae. Fractionation during micro-migration progressively decreases the aromatization of solid bitumen from shale, through tuffaceous and mudstone, to sandy laminae, while increasing light hydrocarbon components and enhancing OM-hosted pore development. The intrasource micro-migration and enrichment of the Chang73 shale oil result from synergistic organic-inorganic diagenesis, with crude oil component fractionation being a key mechanism for forming sweet spots in laminated shale oil reservoirs.
湖相页岩油源内微运移富集微观机制——以鄂尔多斯盆地延长组长73亚段为例
为明确源内页岩油差异富集机理,以鄂尔多斯盆地三叠系延长组3—7段(简称长73亚段)为例,综合运用高分辨率扫描电镜(SEM)、光学显微镜、激光拉曼光谱、岩石热解、有机溶剂萃取等实验手段,对不同成因的固体沥青进行了识别。获得页岩油源内微运移的直接证据,建立页岩纳米/微组构与生油、运移、聚集的耦合关系。长73页岩生烃潜力最大,但热转化率较低。微米级泥质-长英质纹层的频繁交替提高了排烃效率,使原位和迁移固体沥青具有一致的芳香性。富含陆相有机质和粘土矿物的泥岩纹层生烃阈值较低,持烃能力较强,并保留了一定数量的轻质油/沥青,以区分原位沥青和运移沥青的化学结构。凝灰岩和砂质纹层中含有丰富的长英质矿物和迁移沥青。凝灰质纹层在页岩超压作用下发育高角度微裂缝,有利于原油充注到砂质纹层的刚性矿物粒间孔隙中。微运移过程中的分馏作用逐渐降低了页岩、凝灰岩、泥岩、砂质纹层中固体沥青的芳构化程度,同时增加了轻烃组分,增强了有机质孔隙发育。长73页岩油的源内微运移富集是有机-无机协同成岩作用的结果,原油组分分馏是层状页岩油储集层甜点形成的关键机制。
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CiteScore
11.50
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473
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