{"title":"利用有机地球化学、Re-Os 和 U-Pb 地球年代学识别中国西北塔河油田的热液关联石油积累过程","authors":"Shaojie Li, Xiaowen Guo, Bin Wang, Zicheng Cao, Hao Xu, Jiaxu Chen","doi":"10.1306/02132422124","DOIUrl":null,"url":null,"abstract":"The Tahe oil field is one of the largest deeply buried, multistage-charged Paleozoic oil fields in the Tarim Basin, northwestern China. Understanding the temporal evolution of Paleozoic oils is crucial for petroleum prospecting in this region. In this study, a combination of biomarker analysis, stable/radiogenic isotopic analysis, and Re-Os and U-Pb isotope geochronology is used to constrain the timing of oil accumulation in the Tahe oil field. Coexistence of unresolved complex mixture and intact n-alkane series in oil chromatograms suggests the presence of multistage oil accumulation processes in the studied area, and paleo-biodegradation occurred prior to the latest oil charge. Biomarker data show that the source rock for the latest accumulated oils was deposited in a marine reducing–weakly oxidizing environment. An early Permian oil generation event (276 ± 35 Ma) was suggested by Re-Os geochronology. This oil generation event is responsible for the late Permian–Late Triassic charge event (259.9–224.1 Ma), which is identified with in situ U-Pb isotopic analysis of calcites containing primary oil inclusions. These age data provide direct temporal constraints for the latest oil accumulation in the Tahe oil field. Furthermore, C-O-Sr-Os isotopic results show that hydrothermal fluid flowed during this oil accumulation event. Outcomes of this study unravel the Re-Os isotopic analysis of cogenetic crude oils and have the potential of direct dating the latest, hydrothermally linked oil accumulation in multistage-charged deep oil reservoirs.","PeriodicalId":7124,"journal":{"name":"AAPG Bulletin","volume":"61 1","pages":""},"PeriodicalIF":2.7000,"publicationDate":"2024-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Recognition of a hydrothermally linked oil accumulation process in the Tahe oil field, northwestern China, with organic geochemistry, Re-Os, and U-Pb geochronology\",\"authors\":\"Shaojie Li, Xiaowen Guo, Bin Wang, Zicheng Cao, Hao Xu, Jiaxu Chen\",\"doi\":\"10.1306/02132422124\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Tahe oil field is one of the largest deeply buried, multistage-charged Paleozoic oil fields in the Tarim Basin, northwestern China. Understanding the temporal evolution of Paleozoic oils is crucial for petroleum prospecting in this region. In this study, a combination of biomarker analysis, stable/radiogenic isotopic analysis, and Re-Os and U-Pb isotope geochronology is used to constrain the timing of oil accumulation in the Tahe oil field. Coexistence of unresolved complex mixture and intact n-alkane series in oil chromatograms suggests the presence of multistage oil accumulation processes in the studied area, and paleo-biodegradation occurred prior to the latest oil charge. Biomarker data show that the source rock for the latest accumulated oils was deposited in a marine reducing–weakly oxidizing environment. An early Permian oil generation event (276 ± 35 Ma) was suggested by Re-Os geochronology. This oil generation event is responsible for the late Permian–Late Triassic charge event (259.9–224.1 Ma), which is identified with in situ U-Pb isotopic analysis of calcites containing primary oil inclusions. These age data provide direct temporal constraints for the latest oil accumulation in the Tahe oil field. Furthermore, C-O-Sr-Os isotopic results show that hydrothermal fluid flowed during this oil accumulation event. Outcomes of this study unravel the Re-Os isotopic analysis of cogenetic crude oils and have the potential of direct dating the latest, hydrothermally linked oil accumulation in multistage-charged deep oil reservoirs.\",\"PeriodicalId\":7124,\"journal\":{\"name\":\"AAPG Bulletin\",\"volume\":\"61 1\",\"pages\":\"\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"AAPG Bulletin\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1306/02132422124\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"AAPG Bulletin","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1306/02132422124","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Recognition of a hydrothermally linked oil accumulation process in the Tahe oil field, northwestern China, with organic geochemistry, Re-Os, and U-Pb geochronology
The Tahe oil field is one of the largest deeply buried, multistage-charged Paleozoic oil fields in the Tarim Basin, northwestern China. Understanding the temporal evolution of Paleozoic oils is crucial for petroleum prospecting in this region. In this study, a combination of biomarker analysis, stable/radiogenic isotopic analysis, and Re-Os and U-Pb isotope geochronology is used to constrain the timing of oil accumulation in the Tahe oil field. Coexistence of unresolved complex mixture and intact n-alkane series in oil chromatograms suggests the presence of multistage oil accumulation processes in the studied area, and paleo-biodegradation occurred prior to the latest oil charge. Biomarker data show that the source rock for the latest accumulated oils was deposited in a marine reducing–weakly oxidizing environment. An early Permian oil generation event (276 ± 35 Ma) was suggested by Re-Os geochronology. This oil generation event is responsible for the late Permian–Late Triassic charge event (259.9–224.1 Ma), which is identified with in situ U-Pb isotopic analysis of calcites containing primary oil inclusions. These age data provide direct temporal constraints for the latest oil accumulation in the Tahe oil field. Furthermore, C-O-Sr-Os isotopic results show that hydrothermal fluid flowed during this oil accumulation event. Outcomes of this study unravel the Re-Os isotopic analysis of cogenetic crude oils and have the potential of direct dating the latest, hydrothermally linked oil accumulation in multistage-charged deep oil reservoirs.
期刊介绍:
While the 21st-century AAPG Bulletin has undergone some changes since 1917, enlarging to 8 ½ x 11” size to incorporate more material and being published digitally as well as in print, it continues to adhere to the primary purpose of the organization, which is to advance the science of geology especially as it relates to petroleum, natural gas, other subsurface fluids, and mineral resources.
Delivered digitally or in print monthly to each AAPG Member as a part of membership dues, the AAPG Bulletin is one of the most respected, peer-reviewed technical journals in existence, with recent issues containing papers focused on such topics as the Middle East, channel detection, China, permeability, subseismic fault prediction, the U.S., and Africa.