首页|期刊导航|大庆石油地质与开发|塔里木盆地塔河地区奥陶系油气成藏期次差异性及其主控因素

塔里木盆地塔河地区奥陶系油气成藏期次差异性及其主控因素OA

Differences in oil and gas accumulation periods and their main controlling factors in Ordovician Tahe area of Tarim Basin

中文摘要英文摘要

塔里木盆地塔河地区奥陶系具有多期成藏及成藏过程复杂的特征,油气成藏期次差异性及其主控因素尚未揭示,限制了对油气成藏过程的准确认知.基于前人研究成果,综合储层流体包裹体岩相学分析、显微荧光光谱及显微测温,明确了塔河地区奥陶系油气成藏期次差异性及其主控因素.结果表明:塔河地区奥陶系发育3类荧光颜色的油包裹体,并在主峰波长(λmax)及红绿熵值(QF535)上具有明显的差异;结合油包裹体的伴生盐水包裹体的均一温度特征,成藏期次分别对应加里东晚期、海西晚期/燕山期和喜马拉雅期;塔河地区普遍存在3期成藏,而塔河外围地区仅存在2期成藏;从南向北,呈现出第2期油气成藏期北部滞后且主成藏期提前的特征;构造演化差异导致油气成藏期次不同;寒武系烃源岩二次生烃"南早北晚"的差异特征是第2期油气充注北部滞后的根本原因;桑塔木组泥岩盖层和中寒武统膏岩盖层的共同作用控制了主成藏期在空间上的迁移性.研究成果可为后续深入勘探奠定坚实的基础.

Ordovician Tahe area in Tarim Basin is characterized by multi-periods accumulation and complex accu-mulation processes.Differences in oil and gas accumulation periods and their main controlling factors have not been revealed,which restrict the accurate understanding of oil and gas accumulation process.Based on previous re-search,comprehensive analysis of reservoir fluid inclusion petrography,microscopic fluorescence spectroscopy and microscopic temperature measurement is conducted to determine the differences in oil and gas reservoir accumula-tion periods and their main controlling factors in Ordovician Tahe area.The results show that 3 types of fluorescent colors of oil inclusions developed in Ordovician Tahe area,with significant differences in the main peak wavelength(λmax)and red-green entropy value(QF535).Based on the uniform temperature characteristics of associated brine in-clusions in oil inclusions,accumulation periods correspond to the Late Caledonian,Late Hercynian/Yanshanian and Himalayan periods,respectively.Tahe area has generally experienced 3 periods of accumulation,while only 2 periods of accumulation occured in the peripheral areas,with characteristics of the second period of oil and gas ac-cumulation lagged in the north and the main accumulation period gradually becoming earlier from south to north.Differences in structural evolution lead to different periods of oil and gas accumulation.Differential characteristic of secondary hydrocarbon generation of Cambrian source rocks,which is"earlier in the south and later in the north",is the fundamental reason for the lagging of the second period of oil and gas charging in the north.The spatial migra-tion of the main accumulation period is controlled by both mudstone caprock of Santamu Formation and Middle Cam-brian gypsum caprock.The research lays solid foundation for subsequent in-depth exploration.

房柳杉;刘永立;林静文;刘华;苏燕华;王建祥;赵卓扬

中国石化西北油田分公司勘探开发研究院,新疆 乌鲁木齐 830011中国石化西北油田分公司勘探开发研究院,新疆 乌鲁木齐 830011中国石化西北油田分公司勘探开发研究院,新疆 乌鲁木齐 830011中国石油大学(华东)地球科学与技术学院,山东 青岛 266580中国石油大学(华东)地球科学与技术学院,山东 青岛 266580中国石油大学(华东)地球科学与技术学院,山东 青岛 266580中国石油大学(华东)地球科学与技术学院,山东 青岛 266580

能源科技

油气成藏期次成藏差异性深层油气塔里木盆地塔河地区奥陶系

oil and gas accumulation periodaccumulation differencesdeep oil and gasTarim BasinTahe areaOrdovician

《大庆石油地质与开发》 2026 (1)

44-53,10

国家自然科学基金项目"走滑背景下寒武系膏盐岩盖层封闭能力及有效性评价——以塔里木盆地为例"(42172147).

10.19597/J.ISSN.1000-3754.202409042

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