FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4366487503> ?p ?o ?g. }

• W4366487503 endingPage "T579" @default.
• W4366487503 startingPage "T567" @default.
• W4366487503 abstract "Numerous hydrocarbon discoveries in the lower Urho Formation of the western Mahu Slope, China indicate that potential petroliferous reservoirs may exist in that region. However, issues concerning the reservoir characteristics and associated controlling factors remain unclear. To determine the characteristics and associated controlling factors of these reservoirs, we conducted integrated analysis of the 3D seismic volume, wireline logs, mud logs, cores, thin sections, porosity, and permeability data. Several lithologic types were identified from the core, casting thin section, and mud-log data (including mudstone, sandstone, gravity flow-derived glutenite, transitional glutenite, and traction flow-derived glutenite). The contact relationship was determined from the casting thin section data, and it included point contact and lineal contact, followed by concavo-convex contact and suture contact. We found the dominant pore types were found to be intergranular pores, followed by intragranular pores, intramatrix pores, and cracks. The porosity and permeability data reveal that sandstone and traction flow-derived glutenite commonly form low-porosity and low-permeability reservoirs, whereas transitional glutenite commonly forms low-porosity and ultralow-permeability reservoirs and gravity flow-derived glutenite generally forms low-porosity and ultralow-permeability reservoirs. This integrated analysis finds that tectonic movements and a sedimentary environment control the physical properties of the reservoirs. The tectonic movements control reservoir characteristics through thrust fault systems and large-scale provenance, and the sedimentary environment controls reservoir characteristics via facies distribution and lacustrine fluctuation. The insights gained from this study can provide knowledge about the characteristics and associated controlling factors of the reservoirs in the Permian Lower Urho Formation within the western Junggar Basin. These insights can also benefit petroleum reserve and hydrocarbon production exploration in the study area and further petroleum exploration in other areas with similar sedimentary/tectonic settings." @default.
• W4366487503 created "2023-04-22" @default.
• W4366487503 creator A5028813209 @default.
• W4366487503 creator A5038885141 @default.
• W4366487503 creator A5039916179 @default.
• W4366487503 creator A5044269689 @default.
• W4366487503 creator A5046852950 @default.
• W4366487503 creator A5054515233 @default.
• W4366487503 date "2023-06-22" @default.
• W4366487503 modified "2023-09-25" @default.
• W4366487503 title "Characteristics and controlling factors of petroliferous reservoirs in the Permian Lower Urho Formation, western Mahu Slope, Junggar Basin, Northwest China" @default.
• W4366487503 cites W183765136 @default.
• W4366487503 cites W2035432388 @default.
• W4366487503 cites W2081332507 @default.
• W4366487503 cites W2083801410 @default.
• W4366487503 cites W2138821921 @default.
• W4366487503 cites W2488430562 @default.
• W4366487503 cites W2619499711 @default.
• W4366487503 cites W2767235714 @default.
• W4366487503 cites W2782876857 @default.
• W4366487503 cites W2792031555 @default.
• W4366487503 cites W2802138995 @default.
• W4366487503 cites W2926248322 @default.
• W4366487503 cites W2927858183 @default.
• W4366487503 cites W2940276471 @default.
• W4366487503 cites W2995911062 @default.
• W4366487503 cites W2999539945 @default.
• W4366487503 cites W3008797492 @default.
• W4366487503 cites W3086607065 @default.
• W4366487503 cites W3092223958 @default.
• W4366487503 cites W3093401750 @default.
• W4366487503 cites W3127043453 @default.
• W4366487503 cites W3133936150 @default.
• W4366487503 cites W3194989362 @default.
• W4366487503 cites W3201597257 @default.
• W4366487503 cites W3204002104 @default.
• W4366487503 cites W3207632267 @default.
• W4366487503 cites W3207739060 @default.
• W4366487503 cites W4200612917 @default.
• W4366487503 cites W4225146309 @default.
• W4366487503 cites W4283271332 @default.
• W4366487503 cites W4292230017 @default.
• W4366487503 cites W4296198683 @default.
• W4366487503 cites W4298626055 @default.
• W4366487503 doi "https://doi.org/10.1190/int-2022-0122.1" @default.
• W4366487503 hasPublicationYear "2023" @default.
• W4366487503 type Work @default.
• W4366487503 citedByCount "0" @default.
• W4366487503 crossrefType "journal-article" @default.
• W4366487503 hasAuthorship W4366487503A5028813209 @default.
• W4366487503 hasAuthorship W4366487503A5038885141 @default.
• W4366487503 hasAuthorship W4366487503A5039916179 @default.
• W4366487503 hasAuthorship W4366487503A5044269689 @default.
• W4366487503 hasAuthorship W4366487503A5046852950 @default.
• W4366487503 hasAuthorship W4366487503A5054515233 @default.
• W4366487503 hasConcept C109007969 @default.
• W4366487503 hasConcept C114793014 @default.
• W4366487503 hasConcept C120882062 @default.
• W4366487503 hasConcept C122792734 @default.
• W4366487503 hasConcept C127313418 @default.
• W4366487503 hasConcept C130452526 @default.
• W4366487503 hasConcept C146588470 @default.
• W4366487503 hasConcept C151730666 @default.
• W4366487503 hasConcept C17409809 @default.
• W4366487503 hasConcept C187320778 @default.
• W4366487503 hasConcept C2776662147 @default.
• W4366487503 hasConcept C41625074 @default.
• W4366487503 hasConcept C54355233 @default.
• W4366487503 hasConcept C5900021 @default.
• W4366487503 hasConcept C6494504 @default.
• W4366487503 hasConcept C6648577 @default.
• W4366487503 hasConcept C77928131 @default.
• W4366487503 hasConcept C83365034 @default.
• W4366487503 hasConcept C86803240 @default.
• W4366487503 hasConceptScore W4366487503C109007969 @default.
• W4366487503 hasConceptScore W4366487503C114793014 @default.
• W4366487503 hasConceptScore W4366487503C120882062 @default.
• W4366487503 hasConceptScore W4366487503C122792734 @default.
• W4366487503 hasConceptScore W4366487503C127313418 @default.
• W4366487503 hasConceptScore W4366487503C130452526 @default.
• W4366487503 hasConceptScore W4366487503C146588470 @default.
• W4366487503 hasConceptScore W4366487503C151730666 @default.
• W4366487503 hasConceptScore W4366487503C17409809 @default.
• W4366487503 hasConceptScore W4366487503C187320778 @default.
• W4366487503 hasConceptScore W4366487503C2776662147 @default.
• W4366487503 hasConceptScore W4366487503C41625074 @default.
• W4366487503 hasConceptScore W4366487503C54355233 @default.
• W4366487503 hasConceptScore W4366487503C5900021 @default.
• W4366487503 hasConceptScore W4366487503C6494504 @default.
• W4366487503 hasConceptScore W4366487503C6648577 @default.
• W4366487503 hasConceptScore W4366487503C77928131 @default.
• W4366487503 hasConceptScore W4366487503C83365034 @default.
• W4366487503 hasConceptScore W4366487503C86803240 @default.
• W4366487503 hasIssue "3" @default.
• W4366487503 hasLocation W43664875031 @default.
• W4366487503 hasOpenAccess W4366487503 @default.
• W4366487503 hasPrimaryLocation W43664875031 @default.
• W4366487503 hasRelatedWork W2149852641 @default.

• next