Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/890
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dc.contributor.authorallXiaobao, Z.; State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.authorallLiyuan, M.; State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.authorallJianping, C.; The Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of Chinaen
dc.contributor.authorallMingliang, S.; State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.authorallJianqi, T.; The Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of Chinaen
dc.contributor.authorallXiufen, L.; State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.authorallChenpeng, S.; State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.date.accessioned2006-02-22T11:53:42Zen
dc.date.available2006-02-22T11:53:42Zen
dc.date.issued2005en
dc.identifier.urihttp://hdl.handle.net/2122/890en
dc.description.abstractSampled from the Gangxi oil field in the Huanghua depression, Bohaiwan Basin, the crude oil He and Ar isotopic compositions and their geochemical significance were investigated. The result shows that i) the 3He/4He values of the six oil samples free from air contamination indicate a mantle helium contribution ranging between 13.9% and 32.8% and averaging 24.1%, which means that the Gangxi oil field once had a tectonic background of the mantle-derived helium input and higher geothermal flow with an average of 75.0 mWm-2; ii) deduced from the 40Ar/36Ar aging effect the Gangxi oil should be derived from the Tertiary; iii) water injection is the main reason for the air contamination for the Gangxi oil noble gases and the relations between 3He/4He and 4He/20Ne as well as 40Ar/36Ar and 4He/20Ne are of an applicative potential in estimating the water injection effect and the connectivity of producing formations. The search for the crude oil He and Ar isotopes provides a new approach to inferring natural gas and oil sources, tectonic backgrounds, geothermal flow and water injection effect.en
dc.format.extent666986 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameINGVen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries1/48 (2005)en
dc.subjectcrude oilen
dc.subjectnoble gas tracingen
dc.subjectGangxi oil fielden
dc.subjectHuanghua depressionen
dc.titleCrude oil He and Ar isotopic characteristics and their geochemical significance: an example from the Gangxi oil field in the Huanghua depressionen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorXiaobao, Z.en
dc.contributor.authorLiyuan, M.en
dc.contributor.authorJianping, C.en
dc.contributor.authorMingliang, S.en
dc.contributor.authorJianqi, T.en
dc.contributor.authorXiufen, L.en
dc.contributor.authorChenpeng, S.en
dc.contributor.departmentState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.departmentState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.departmentThe Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of Chinaen
dc.contributor.departmentState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.departmentThe Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of Chinaen
dc.contributor.departmentState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
dc.contributor.departmentState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of Chinaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of China-
crisitem.author.deptState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of China-
crisitem.author.deptThe Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of China-
crisitem.author.deptState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of China-
crisitem.author.deptThe Research Institute of Exploration and Development,China National Petroleum Corporation, Beijing, People s Republic of China-
crisitem.author.deptState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of China-
crisitem.author.deptState Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology,Chinese Academy of Sciences, Gansu, People s Republic of China-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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