FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022359608> ?p ?o ?g. }

• W2022359608 endingPage "104" @default.
• W2022359608 startingPage "88" @default.
• W2022359608 abstract "Oil and gas resources are abundant in China’s continental sedimentary basins, where the main task of exploration has been finding oil for many years. In recent years, however, new discoveries of large-scale natural gas have been successively obtained. The natural gas mainly exists in the sedimentary association of alternated mudstones and tight sandstones and is dominantly low-permeability tight sand gas. Through the in-depth study on gas reservoir analysis, diagenetic evolution, source rock distribution and hydrocarbon-generating behavior, natural gas generation and accumulation, it is concluded that, during the major subsiding stage of large scale lake basins, the multicyclic subsiding process of the lake surface controls the development of high quality source rocks, the wide distribution of sands, and the superimposition of the two types of rocks in the vertical direction. The lacustrine muddy source rocks are developed, including mud shale, carbonaceous mudstone and coal bed which are in the medium–high evolution stage and produce mainly gas and the gas generation intensity is high. Through the analysis of the subsidence evolution processes of the Carboniferous–Permian Systems (transitional marine–continental facies) in the Ordos Basin and the Triassic Xujiahe Formation (continental facies) in the Sichuan Basin, it is concluded that the widely distributed sandbodies of delta facies, although with tight properties, are interbedded with source rocks and easy to accumulate natural gases. The natural gas is migrated and accumulated within small distance, and is characterized by large-area accumulation. Because of the strong hydrocarbon generation capacity, big thickness and stable distribution of the underlying mud shale, the potential of gas resources should not be underestimated. The geocyclicity of China’s continental sedimentary basins controls the sedimentary association of alternated mudstones and tight sandstones, resulting in superimposed accumulations of shale gas and tight sand gas." @default.
• W2022359608 created "2016-06-24" @default.
• W2022359608 creator A5027013375 @default.
• W2022359608 creator A5057195398 @default.
• W2022359608 creator A5061602320 @default.
• W2022359608 creator A5070031719 @default.
• W2022359608 creator A5072451542 @default.
• W2022359608 creator A5075645045 @default.
• W2022359608 creator A5085341178 @default.
• W2022359608 date "2012-05-01" @default.
• W2022359608 modified "2023-10-01" @default.
• W2022359608 title "Sedimentary association of alternated mudstones and tight sandstones in China’s oil and gas bearing basins and its natural gas accumulation" @default.
• W2022359608 cites W13340261 @default.
• W2022359608 cites W1550362504 @default.
• W2022359608 cites W1963574048 @default.
• W2022359608 cites W1970826038 @default.
• W2022359608 cites W1993416152 @default.
• W2022359608 cites W2043082514 @default.
• W2022359608 cites W2071384249 @default.
• W2022359608 cites W2078617700 @default.
• W2022359608 cites W2079240626 @default.
• W2022359608 cites W2082129271 @default.
• W2022359608 cites W2090576064 @default.
• W2022359608 cites W2105549435 @default.
• W2022359608 cites W2110946462 @default.
• W2022359608 cites W2113464319 @default.
• W2022359608 cites W2123573076 @default.
• W2022359608 cites W2128802367 @default.
• W2022359608 doi "https://doi.org/10.1016/j.jseaes.2012.01.008" @default.
• W2022359608 hasPublicationYear "2012" @default.
• W2022359608 type Work @default.
• W2022359608 sameAs 2022359608 @default.
• W2022359608 citedByCount "45" @default.
• W2022359608 countsByYear W20223596082013 @default.
• W2022359608 countsByYear W20223596082014 @default.
• W2022359608 countsByYear W20223596082015 @default.
• W2022359608 countsByYear W20223596082016 @default.
• W2022359608 countsByYear W20223596082017 @default.
• W2022359608 countsByYear W20223596082018 @default.
• W2022359608 countsByYear W20223596082019 @default.
• W2022359608 countsByYear W20223596082020 @default.
• W2022359608 countsByYear W20223596082021 @default.
• W2022359608 countsByYear W20223596082022 @default.
• W2022359608 countsByYear W20223596082023 @default.
• W2022359608 crossrefType "journal-article" @default.
• W2022359608 hasAuthorship W2022359608A5027013375 @default.
• W2022359608 hasAuthorship W2022359608A5057195398 @default.
• W2022359608 hasAuthorship W2022359608A5061602320 @default.
• W2022359608 hasAuthorship W2022359608A5070031719 @default.
• W2022359608 hasAuthorship W2022359608A5072451542 @default.
• W2022359608 hasAuthorship W2022359608A5075645045 @default.
• W2022359608 hasAuthorship W2022359608A5085341178 @default.
• W2022359608 hasConcept C109007969 @default.
• W2022359608 hasConcept C114793014 @default.
• W2022359608 hasConcept C126559015 @default.
• W2022359608 hasConcept C127313418 @default.
• W2022359608 hasConcept C130452526 @default.
• W2022359608 hasConcept C146588470 @default.
• W2022359608 hasConcept C151730666 @default.
• W2022359608 hasConcept C17409809 @default.
• W2022359608 hasConcept C178790620 @default.
• W2022359608 hasConcept C185592680 @default.
• W2022359608 hasConcept C200646496 @default.
• W2022359608 hasConcept C2777447996 @default.
• W2022359608 hasConcept C2779096232 @default.
• W2022359608 hasConcept C5900021 @default.
• W2022359608 hasConcept C59427239 @default.
• W2022359608 hasConcept C6494504 @default.
• W2022359608 hasConcept C83365034 @default.
• W2022359608 hasConceptScore W2022359608C109007969 @default.
• W2022359608 hasConceptScore W2022359608C114793014 @default.
• W2022359608 hasConceptScore W2022359608C126559015 @default.
• W2022359608 hasConceptScore W2022359608C127313418 @default.
• W2022359608 hasConceptScore W2022359608C130452526 @default.
• W2022359608 hasConceptScore W2022359608C146588470 @default.
• W2022359608 hasConceptScore W2022359608C151730666 @default.
• W2022359608 hasConceptScore W2022359608C17409809 @default.
• W2022359608 hasConceptScore W2022359608C178790620 @default.
• W2022359608 hasConceptScore W2022359608C185592680 @default.
• W2022359608 hasConceptScore W2022359608C200646496 @default.
• W2022359608 hasConceptScore W2022359608C2777447996 @default.
• W2022359608 hasConceptScore W2022359608C2779096232 @default.
• W2022359608 hasConceptScore W2022359608C5900021 @default.
• W2022359608 hasConceptScore W2022359608C59427239 @default.
• W2022359608 hasConceptScore W2022359608C6494504 @default.
• W2022359608 hasConceptScore W2022359608C83365034 @default.
• W2022359608 hasLocation W20223596081 @default.
• W2022359608 hasOpenAccess W2022359608 @default.
• W2022359608 hasPrimaryLocation W20223596081 @default.
• W2022359608 hasRelatedWork W1999255135 @default.
• W2022359608 hasRelatedWork W2263691624 @default.
• W2022359608 hasRelatedWork W2362747183 @default.
• W2022359608 hasRelatedWork W2365846915 @default.
• W2022359608 hasRelatedWork W2378348218 @default.
• W2022359608 hasRelatedWork W2379281178 @default.
• W2022359608 hasRelatedWork W2392364919 @default.
• W2022359608 hasRelatedWork W2594306655 @default.
• W2022359608 hasRelatedWork W3142466752 @default.

• next