FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2365199462> ?p ?o ?g. }

• W2365199462 abstract "There are four generative hydrocarbon source rocks of Carboniferous, Permian, Triassic, and Jurassic age in the east of the Junggar Basin. This geochemical study has shown that Permian source rocks, which contain high abundance of organic matter with good genetic potential, are the best hydrocarbon source rocks in this area. Triassic source rocks are shown to be next best in these aspects. The abundance of mainly type I organic matter in Jurassic and Carboniferous source rocks varies greatly, and their genetic potential is lower than that of Permian and Triassic rocks. These four source rock units in the Fukang sag all reach a mature to high mature stage and have generated large amounts of oil. Using carbon isotopic and biomarker data, the crude oils in this area can be divided into five groups. The first group of crude oils is derived from the Permian, the second group from the Triassic, and the third group from the Jurassic source rocks. The geochemical properties of the fourth group of oils are intermediate between the properties of typical Permian, Triassic and Jurassic oils. The fifth group of crude oils is particularly isotopically heavy, and originate from Carboniferous source rocks. The crude oils in the Cainan field belong to the fourth group of oil, and are of a special type in that they have little correlation with any of the four known source rocks in the basin. Based on their distribution in the reservoir formations, and their carbon isotopic and biomarker compositions, it is concluded that these crude oils are mixtures of hydrocarbons from Permian, Triassic and Jurassic source rocks. A mixing calculation using whole-oil stable carbon isotope ratios of typical end-member crude oils suggests that the contribution of Jurassic source rocks to the Cainan crude oils averages around 60%. A second calculation based on absolute concentrations of biomarkers indicates that the Jurassic contribution averages 62%, while those of the Triassic and Permian source rocks average 15% and 23%, respectively. Artificial laboratory mixing of three typical 60% Permian oil, 20% Triassic oil and 20% Jurassic oils indicates that the mixture has similar geochemical features. In summary, the crude oils in the Cainan oilfield are typical mixed oil, and mainly derived from Jurassic source rocks in the Fukarig Sag." @default.
• W2365199462 created "2016-06-24" @default.
• W2365199462 creator A5011571888 @default.
• W2365199462 date "2004-01-01" @default.
• W2365199462 modified "2023-09-24" @default.
• W2365199462 title "The Cainan Oilfield: A Typical Mixed Crude Oil of Three-endmember" @default.
• W2365199462 hasPublicationYear "2004" @default.
• W2365199462 type Work @default.
• W2365199462 sameAs 2365199462 @default.
• W2365199462 citedByCount "0" @default.
• W2365199462 crossrefType "journal-article" @default.
• W2365199462 hasAuthorship W2365199462A5011571888 @default.
• W2365199462 hasConcept C109007969 @default.
• W2365199462 hasConcept C126559015 @default.
• W2365199462 hasConcept C127313418 @default.
• W2365199462 hasConcept C149918038 @default.
• W2365199462 hasConcept C151730666 @default.
• W2365199462 hasConcept C17409809 @default.
• W2365199462 hasConcept C178790620 @default.
• W2365199462 hasConcept C185592680 @default.
• W2365199462 hasConcept C2781311116 @default.
• W2365199462 hasConcept C83365034 @default.
• W2365199462 hasConceptScore W2365199462C109007969 @default.
• W2365199462 hasConceptScore W2365199462C126559015 @default.
• W2365199462 hasConceptScore W2365199462C127313418 @default.
• W2365199462 hasConceptScore W2365199462C149918038 @default.
• W2365199462 hasConceptScore W2365199462C151730666 @default.
• W2365199462 hasConceptScore W2365199462C17409809 @default.
• W2365199462 hasConceptScore W2365199462C178790620 @default.
• W2365199462 hasConceptScore W2365199462C185592680 @default.
• W2365199462 hasConceptScore W2365199462C2781311116 @default.
• W2365199462 hasConceptScore W2365199462C83365034 @default.
• W2365199462 hasLocation W23651994621 @default.
• W2365199462 hasOpenAccess W2365199462 @default.
• W2365199462 hasPrimaryLocation W23651994621 @default.
• W2365199462 hasRelatedWork W1968646058 @default.
• W2365199462 hasRelatedWork W2002388115 @default.
• W2365199462 hasRelatedWork W2002624630 @default.
• W2365199462 hasRelatedWork W2017702573 @default.
• W2365199462 hasRelatedWork W2061749069 @default.
• W2365199462 hasRelatedWork W2068910602 @default.
• W2365199462 hasRelatedWork W2078231276 @default.
• W2365199462 hasRelatedWork W2354865869 @default.
• W2365199462 hasRelatedWork W2358866504 @default.
• W2365199462 hasRelatedWork W2366885048 @default.
• W2365199462 hasRelatedWork W2370905801 @default.
• W2365199462 hasRelatedWork W2372130013 @default.
• W2365199462 hasRelatedWork W2375283044 @default.
• W2365199462 hasRelatedWork W2375386223 @default.
• W2365199462 hasRelatedWork W2391684398 @default.
• W2365199462 hasRelatedWork W2392412279 @default.
• W2365199462 hasRelatedWork W2392972470 @default.
• W2365199462 hasRelatedWork W2527376192 @default.
• W2365199462 hasRelatedWork W2623787740 @default.
• W2365199462 hasRelatedWork W3092715086 @default.
• W2365199462 isParatext "false" @default.
• W2365199462 isRetracted "false" @default.
• W2365199462 magId "2365199462" @default.
• W2365199462 workType "article" @default.