首页|期刊导航|石油勘探与开发|陆相页岩油阶段充注-累积充注模式与分异聚集

陆相页岩油阶段充注-累积充注模式与分异聚集OA

Staged-cumulative charging and differential accumulation of continental shale oil:A case study of Permian Lucaogou Formation shale oil in Junggar Basin,NW China

中文摘要英文摘要

准噶尔盆地吉木萨尔凹陷二叠系芦草沟组上、下甜点段原油性质存在"轻重反转"现象,且与油岩成熟度不匹配.为更加科学地诠释上述异常地质现象,综合地质、地球化学与岩石物理数据资料,从热成熟度、有机相、润湿性、异常高压及运移分馏等方面进行了系统剖析.研究取得以下进展:提出"阶段充注-累积充注"模式,用于解释湖相页岩油性质差异;指出生物标志物耗减程度、油气充注历史以及源-储体系开放度共同控制原油组成,而非单一受控于热成熟度或有机相带等因素.其中,上甜点段在早期为半开放体系,烃类生成与排出基本同步,早期生成的富生物标志物重质组分优先排出,晚期因页岩致密化导致高成熟轻质烃滞留;而下甜点段则为相对封闭体系,多期生成烃类持续累积混合保存,叠加作用削弱甾烷异构化信号,难以真实反映各期及最终热成熟度.这一认识合理解释了低成熟或成熟度相近层段中生物标志物参数异常偏低或失真的现象.该充注模式阐明了原油性质的反转机制,并将研究重心由静态成熟度判识转向充注动力学过程,为揭示湖相页岩油成藏地质规律、指导甜点优选与勘探开发部署提供了新的理论依据.

In the Jimusaer Sag of the Junggar Basin,crude oils from the upper and lower sweet-spot intervals of the Permian Lucaogou Formation display a pronounced"light-heavy reversal"in oil properties that indicates a fundamental mismatch between oil composition and maturity rock.To resolve this anomaly,this study integrates geological,geochemical,and petrophysical datasets and systematically evaluates the combined roles of thermal evolution,organic facies,wettability,abnormal overpressure,and migration-related fractionation on shale oil composition.On this basis,a"staged charging-cumulative charging"model is proposed to explain compositional heterogeneity in lacustrine shale oils.The results demonstrate that crude-oil composition are jointly controlled by the extent of biomarker depletion,the temporal evolution of hydrocarbon charging,and the openness of the source-reservoir system,rather than by thermal maturity or organic facies alone.The upper sweet-spot interval is interpreted to have functioned as a semi-open system during early stages,in which hydrocarbon generation and expulsion were broadly synchronous,leading to preferential loss of early-generated,biomarker-rich heavy components,whereas progressive shale densification at later stages promoted the retention of highly mature,light hydrocarbons.In contrast,the lower sweet-spot interval represents a relatively closed system,where hydrocarbons generated during multiple stages continuously accumulated and were preserved as mixed charges;superposition of multi-phase fluids progressively weakened sterane isomerization signals,rendering them unreliable indicators of individual charging events or final thermal maturity.This charging behavior provides a reasonable explanation for anomalously low or distorted biomarker parameters observed in intervals of low or similar maturity.Overall,the proposed charging model reconciles the observed reversal in crude-oil properties and,by shifting the interpretive focus from static maturity assessment to charging dynamics,offers a new theoretical basis for understanding lacustrine shale oil accumulation processes,and guiding sweet-spot selection and exploration-development strategies.

黄海平;张鸿;马勇

卡尔加里大学地球、能源与环境学院,卡尔加里T2N1N4,加拿大||长江大学地球科学学院,武汉 430100中国地质大学(北京)能源学院,北京 100083中国石油大学(北京)油气资源与工程国家重点实验室,北京 102249

能源科技

页岩油差异性烃源岩成熟度原油成熟度阶段充注-累积充注滞留动力学芦草沟组吉木萨尔凹陷准噶尔盆地

shale oil heterogeneitysource rock maturityoil maturitystaged-cumulative chargeretention dynamicsLucaogou FormationJimusaer SagJunggar Basin

《石油勘探与开发》 2026 (1)

81-93,13

国家自然科学基金项目(42173030,42302161,42473034)科学技术部新型油气勘探开发国家科技重大专项(2025ZD1400803)

10.11698/PED.202500136SD

评论