FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1950147882> ?p ?o ?g. }

• W1950147882 endingPage "1026" @default.
• W1950147882 startingPage "1014" @default.
• W1950147882 abstract "Tight oil in the Permian Tiaohu Formation in the Santanghu Basin, northwest China, has a peculiar property such that the reservoir is sedimentary organic matter-bearing tuff characterized by high porosity (10%–25%) and very low permeability, mainly in the range of 0.01–0.50 mD. Biomarker and stable carbon isotope compositions of selected crude oils and source-rock extracts were analyzed to determine the source rock of the tight oil. Source rocks in the Lucaogou Formation consist of various rock types dominated by mudstones containing organic matter with intense yellow–green fluorescence. Mudstones in the Lucaogou Formation have total organic carbon (TOC) values mainly in the range of 1.0–8.0 wt%, hydrocarbon generation potential (S 1 + S 2 ) mostly >6 mg/g, and chloroform extractable bitumen “A” generally >0.1%. The maceral composition is predominantly fluorescing amorphinite. The hydrogen index (HI) varies from 300 to 900 mg HC/g TOC, indicating dominant Type I and Type II kerogen. Compared with the mudstones and tuffs in the Tiaohu Formation, the mudstones in the Lucaogou Formation are the best source rocks. The biomarker characteristics of mudstone extracts in the Lucaogou Formation differ from those in the Tiaohu Formation, based on the gammacerane index, β-carotane content, and the relative contents of C 27 , C 28 , and C 29 regular steranes. Crude oil samples in the tuff show low pristane/phytane (Pr/Ph) ratios, high gammacerane indices, high β-carotane, and a dominance of the C 29 regular sterane followed by C 28 and C 27 steranes, as well as depleted stable carbon isotope compositions. Oil–source correlation with biomarkers and δ 13 C values shows that the crude oil in the tuffs mainly originates from underlying source rocks in the Lucaogou Formation. The sedimentary organic matter in the tuffs also makes a small contribution to the tuffaceous reservoir. Therefore, the tuffaceous tight reservoir in the Tiaohu Formation is unusual in that the oil is not indigenous; rather, it migrates a long distance to accumulate in the upper reservoir." @default.
• W1950147882 created "2016-06-24" @default.
• W1950147882 creator A5009799305 @default.
• W1950147882 creator A5013473393 @default.
• W1950147882 creator A5087222691 @default.
• W1950147882 creator A5089032405 @default.
• W1950147882 date "2015-11-01" @default.
• W1950147882 modified "2023-10-16" @default.
• W1950147882 title "Oil–source rock correlation for tight oil in tuffaceous reservoirs in the Permian Tiaohu Formation, Santanghu Basin, northwest China" @default.
• W1950147882 cites W142464504 @default.
• W1950147882 cites W1963641066 @default.
• W1950147882 cites W1968450376 @default.
• W1950147882 cites W1980995270 @default.
• W1950147882 cites W1991111724 @default.
• W1950147882 cites W1997338331 @default.
• W1950147882 cites W1998468359 @default.
• W1950147882 cites W2012441546 @default.
• W1950147882 cites W2014489970 @default.
• W1950147882 cites W2020119617 @default.
• W1950147882 cites W2020388968 @default.
• W1950147882 cites W2020931994 @default.
• W1950147882 cites W2025466026 @default.
• W1950147882 cites W2025851260 @default.
• W1950147882 cites W2035288181 @default.
• W1950147882 cites W2038406275 @default.
• W1950147882 cites W2045386399 @default.
• W1950147882 cites W2048992833 @default.
• W1950147882 cites W2049626686 @default.
• W1950147882 cites W2052794190 @default.
• W1950147882 cites W2053531749 @default.
• W1950147882 cites W2056160475 @default.
• W1950147882 cites W2062391313 @default.
• W1950147882 cites W2066980677 @default.
• W1950147882 cites W2090122760 @default.
• W1950147882 cites W2105621431 @default.
• W1950147882 cites W2112109341 @default.
• W1950147882 cites W2117572389 @default.
• W1950147882 cites W2117581153 @default.
• W1950147882 cites W2130733762 @default.
• W1950147882 cites W2136322272 @default.
• W1950147882 cites W2141599763 @default.
• W1950147882 cites W2151566944 @default.
• W1950147882 cites W2151829974 @default.
• W1950147882 cites W2152917047 @default.
• W1950147882 cites W2154446767 @default.
• W1950147882 cites W2159160498 @default.
• W1950147882 cites W2162457106 @default.
• W1950147882 cites W2323611142 @default.
• W1950147882 cites W4205550164 @default.
• W1950147882 doi "https://doi.org/10.1139/cjes-2015-0055" @default.
• W1950147882 hasPublicationYear "2015" @default.
• W1950147882 type Work @default.
• W1950147882 sameAs 1950147882 @default.
• W1950147882 citedByCount "24" @default.
• W1950147882 countsByYear W19501478822016 @default.
• W1950147882 countsByYear W19501478822018 @default.
• W1950147882 countsByYear W19501478822019 @default.
• W1950147882 countsByYear W19501478822020 @default.
• W1950147882 countsByYear W19501478822021 @default.
• W1950147882 countsByYear W19501478822022 @default.
• W1950147882 countsByYear W19501478822023 @default.
• W1950147882 crossrefType "journal-article" @default.
• W1950147882 hasAuthorship W1950147882A5009799305 @default.
• W1950147882 hasAuthorship W1950147882A5013473393 @default.
• W1950147882 hasAuthorship W1950147882A5087222691 @default.
• W1950147882 hasAuthorship W1950147882A5089032405 @default.
• W1950147882 hasConcept C107872376 @default.
• W1950147882 hasConcept C109007969 @default.
• W1950147882 hasConcept C126559015 @default.
• W1950147882 hasConcept C127313418 @default.
• W1950147882 hasConcept C151730666 @default.
• W1950147882 hasConcept C153127940 @default.
• W1950147882 hasConcept C158787203 @default.
• W1950147882 hasConcept C167195282 @default.
• W1950147882 hasConcept C17409809 @default.
• W1950147882 hasConcept C178790620 @default.
• W1950147882 hasConcept C185592680 @default.
• W1950147882 hasConcept C199289684 @default.
• W1950147882 hasConcept C2776141960 @default.
• W1950147882 hasConcept C2779196632 @default.
• W1950147882 hasConcept C2780888746 @default.
• W1950147882 hasConcept C30370900 @default.
• W1950147882 hasConcept C48743137 @default.
• W1950147882 hasConcept C59235061 @default.
• W1950147882 hasConcept C6494504 @default.
• W1950147882 hasConceptScore W1950147882C107872376 @default.
• W1950147882 hasConceptScore W1950147882C109007969 @default.
• W1950147882 hasConceptScore W1950147882C126559015 @default.
• W1950147882 hasConceptScore W1950147882C127313418 @default.
• W1950147882 hasConceptScore W1950147882C151730666 @default.
• W1950147882 hasConceptScore W1950147882C153127940 @default.
• W1950147882 hasConceptScore W1950147882C158787203 @default.
• W1950147882 hasConceptScore W1950147882C167195282 @default.
• W1950147882 hasConceptScore W1950147882C17409809 @default.
• W1950147882 hasConceptScore W1950147882C178790620 @default.
• W1950147882 hasConceptScore W1950147882C185592680 @default.
• W1950147882 hasConceptScore W1950147882C199289684 @default.
• W1950147882 hasConceptScore W1950147882C2776141960 @default.

• next