The organic matter(OM)enrichment mechanisms and depositional environment characteristics of lacustrine source rocks in the western Bozhong Sag,Bohai Bay Basin in Northeast China remain controversial.To address these i...The organic matter(OM)enrichment mechanisms and depositional environment characteristics of lacustrine source rocks in the western Bozhong Sag,Bohai Bay Basin in Northeast China remain controversial.To address these issues,based on Rock-Eval pyrolysis,kerogen macerals,H/C and O/C ratios,GC-MS,major and trace elements,the Dongying Formation Member(Mbr)3(E_(3)d_(3)),the Shahejie Formation mbrs 1 and 2(E_(2)s_(1+2)),and the Shahejie Mbr 3(E_(2)s_(3))source rocks in the western Bozhong Sag were studied.The above methods were used to reveal their geochemical properties,OM origins and depositional environments,all of which indicate that E_(2)s_(1+2)and E_(2)s_(3)are excellent source rocks,and that E_(3)d_(3)is of the second good quality.E_(3)d_(3)source rocks were formed under a warm and humid climate,mainly belong to fluvial/delta facies,the E_(3)d_(3)sediments formed under weakly oxidizing and freshwater conditions.Comparatively,the depositional environments of E_(2)s_(1+2)source rocks were arid and cold climate,representing saline or freshwater lacustrine facies,and the sediments of E_(2)s_(1+2)belong to anoxic or suboxic settings with large evaporation and salinity.During the period of E_(2)s_(3),the climate became warm and humid,indicating the freshwater lacustrine facies,and E_(2)s_(3)was characterized by freshwater and abundant algae.Moreover,compared with other intervals,the OM origin of E_(3)d_(3)source rocks has noticeable terrestrial input.The OM origin of the E_(2)s_(1+2)and E_(2)s_(3)are mainly plankton and bacteria.Tectonic subsidence and climate change have affected the changes of the depositional environment in the western Bozhong Sag,thus controlling the distribution of the source rocks,the geochemical characteristics in the three intervals of lacustrine source rocks have distinct differences.Overall,these factors are effective to evaluate the paleoenvironmental characteristics of source rocks by biomarkers,major and trace elements.The established models may have positive implications for research of lacustrine source rocks in offshore areas with few drillings.展开更多
利用三维地震和钻井资料对辽西凹陷锦州20-2北油田古近系沙河街组第二段油气的烃源岩、储层、圈闭、运移、保存条件及成藏过程进行系统研究。结果表明:(1)锦州20-2北油田沙二段储层具有辽中北洼和辽西北洼“双洼多源”供烃的优势;(2)沙...利用三维地震和钻井资料对辽西凹陷锦州20-2北油田古近系沙河街组第二段油气的烃源岩、储层、圈闭、运移、保存条件及成藏过程进行系统研究。结果表明:(1)锦州20-2北油田沙二段储层具有辽中北洼和辽西北洼“双洼多源”供烃的优势;(2)沙二段储层沉积微相包括水下分流河道和河口坝,大多具中孔-中渗特征,区域盖层为上覆半深湖-深湖相厚层泥岩,储盖组合条件优越;(3)该油田为依附于辽西三号断层并被其派生断层切割形成的一个典型断块圈闭群,在挤压应力背景下,油田处于构造相对高部位,运移条件良好,同时受挤压应力影响,控圈断层闭合度高,保存条件良好;(4)沙二段油气具2期成藏的特征,早期为馆陶组沉积时期(23.3~12 Ma B.P.),晚期为平原组沉积时期(2.6 Ma B.P.至今),其中晚期为油气大规模充注时期。锦州20-2北油田沙二段油气成藏条件优越,主要为晚期充注成藏。展开更多
基金funded by the“Key Scientific Issues and Innovative Technology Research on Oil and Gas Resource Exploration in China Sea Risk Exploration Area”(Grant No.CCL2022RCPS2017XNN)from CNOOC Research Institute,Beijing.
文摘The organic matter(OM)enrichment mechanisms and depositional environment characteristics of lacustrine source rocks in the western Bozhong Sag,Bohai Bay Basin in Northeast China remain controversial.To address these issues,based on Rock-Eval pyrolysis,kerogen macerals,H/C and O/C ratios,GC-MS,major and trace elements,the Dongying Formation Member(Mbr)3(E_(3)d_(3)),the Shahejie Formation mbrs 1 and 2(E_(2)s_(1+2)),and the Shahejie Mbr 3(E_(2)s_(3))source rocks in the western Bozhong Sag were studied.The above methods were used to reveal their geochemical properties,OM origins and depositional environments,all of which indicate that E_(2)s_(1+2)and E_(2)s_(3)are excellent source rocks,and that E_(3)d_(3)is of the second good quality.E_(3)d_(3)source rocks were formed under a warm and humid climate,mainly belong to fluvial/delta facies,the E_(3)d_(3)sediments formed under weakly oxidizing and freshwater conditions.Comparatively,the depositional environments of E_(2)s_(1+2)source rocks were arid and cold climate,representing saline or freshwater lacustrine facies,and the sediments of E_(2)s_(1+2)belong to anoxic or suboxic settings with large evaporation and salinity.During the period of E_(2)s_(3),the climate became warm and humid,indicating the freshwater lacustrine facies,and E_(2)s_(3)was characterized by freshwater and abundant algae.Moreover,compared with other intervals,the OM origin of E_(3)d_(3)source rocks has noticeable terrestrial input.The OM origin of the E_(2)s_(1+2)and E_(2)s_(3)are mainly plankton and bacteria.Tectonic subsidence and climate change have affected the changes of the depositional environment in the western Bozhong Sag,thus controlling the distribution of the source rocks,the geochemical characteristics in the three intervals of lacustrine source rocks have distinct differences.Overall,these factors are effective to evaluate the paleoenvironmental characteristics of source rocks by biomarkers,major and trace elements.The established models may have positive implications for research of lacustrine source rocks in offshore areas with few drillings.
文摘利用三维地震和钻井资料对辽西凹陷锦州20-2北油田古近系沙河街组第二段油气的烃源岩、储层、圈闭、运移、保存条件及成藏过程进行系统研究。结果表明:(1)锦州20-2北油田沙二段储层具有辽中北洼和辽西北洼“双洼多源”供烃的优势;(2)沙二段储层沉积微相包括水下分流河道和河口坝,大多具中孔-中渗特征,区域盖层为上覆半深湖-深湖相厚层泥岩,储盖组合条件优越;(3)该油田为依附于辽西三号断层并被其派生断层切割形成的一个典型断块圈闭群,在挤压应力背景下,油田处于构造相对高部位,运移条件良好,同时受挤压应力影响,控圈断层闭合度高,保存条件良好;(4)沙二段油气具2期成藏的特征,早期为馆陶组沉积时期(23.3~12 Ma B.P.),晚期为平原组沉积时期(2.6 Ma B.P.至今),其中晚期为油气大规模充注时期。锦州20-2北油田沙二段油气成藏条件优越,主要为晚期充注成藏。
