FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4293493780> ?p ?o ?g. }

• W4293493780 endingPage "10885" @default.
• W4293493780 startingPage "10870" @default.
• W4293493780 abstract "Among the shale gas fields in the Sichuan Basin, the Fuling, Changning, and Weiyuan fields with Wufeng Formation-Longmaxi Formation as the target formation have made significant contributions to the shale gas industry in China. However, several other areas in the basin which have witnessed gas flow from wildcat wells have not realized commercial development. In this study, we analyzed the Wufeng Formation–Longmaxi Formation shale gas reservoirs from the perspective of a coupling mechanism of source and seal, by considering three aspects, including the characteristics of source and cap rocks, evolution history of the source rock–reservoir caprock, and the differential enrichment of shale gas. The results indicate the following: (1) The occurrence of the regional caprock (Triassic gypsum-salt) determines the distribution of overpressured and normally pressured shale gas reservoirs. In addition, the erosion of the caprock and its integrity control the gas content and cost-efficiency of the normally pressured shale gas reservoirs. (2) For the overpressured reservoirs, the thickness of the siliceous and carbonate-bearing siliceous shales in the WF2-LM4 graptolite zone determines the gas content and producibility of the lower shale gas layer. In terms of the upper layers, the structural form plays a critical role. Generally, gas reservoirs in the upper layers that occupy the higher part of an anticline are more favorable, whereas those in a syncline or monocline exhibit poor productivity. (3) For the normally pressured shale gas reservoirs with poor caprock integrity, the enrichment and the commercial value of the gas depend mostly on the thickness of the WF2-LM4 graptolite zone. Therefore, we conclude that the areas near the core of synclines are more favorable and structurally stable, with relatively high formation pressure and moderate burial depths. Our findings can improve sweet spot prediction and offer valuable guidance for shale gas development in China and globally." @default.
• W4293493780 created "2022-08-29" @default.
• W4293493780 creator A5010596687 @default.
• W4293493780 creator A5063285358 @default.
• W4293493780 date "2022-08-29" @default.
• W4293493780 modified "2023-10-14" @default.
• W4293493780 title "Evolution History of Overpressured and Normally Pressured Shale Gas Reservoirs in Wufeng Formation–Longmaxi Formation, Sichuan Basin, China: An Analysis from the Perspective of Source and Seal Coupling Mechanism" @default.
• W4293493780 cites W1965127836 @default.
• W4293493780 cites W2125435197 @default.
• W4293493780 cites W2161051067 @default.
• W4293493780 cites W2163736333 @default.
• W4293493780 cites W2290720069 @default.
• W4293493780 cites W2326312167 @default.
• W4293493780 cites W2339191110 @default.
• W4293493780 cites W2469078927 @default.
• W4293493780 cites W2600785804 @default.
• W4293493780 cites W2607816345 @default.
• W4293493780 cites W2758763225 @default.
• W4293493780 cites W2782179144 @default.
• W4293493780 cites W2784283637 @default.
• W4293493780 cites W2793458647 @default.
• W4293493780 cites W2806674185 @default.
• W4293493780 cites W2878411687 @default.
• W4293493780 cites W2964935799 @default.
• W4293493780 cites W2966038816 @default.
• W4293493780 cites W2966855531 @default.
• W4293493780 cites W3014587844 @default.
• W4293493780 cites W3028180615 @default.
• W4293493780 cites W3029555420 @default.
• W4293493780 cites W3041369387 @default.
• W4293493780 cites W3094499785 @default.
• W4293493780 cites W3114984328 @default.
• W4293493780 cites W3130420781 @default.
• W4293493780 cites W3132678942 @default.
• W4293493780 cites W3138999950 @default.
• W4293493780 cites W3165130236 @default.
• W4293493780 cites W3171311538 @default.
• W4293493780 cites W3212774118 @default.
• W4293493780 doi "https://doi.org/10.1021/acs.energyfuels.2c01925" @default.
• W4293493780 hasPublicationYear "2022" @default.
• W4293493780 type Work @default.
• W4293493780 citedByCount "8" @default.
• W4293493780 countsByYear W42934937802023 @default.
• W4293493780 crossrefType "journal-article" @default.
• W4293493780 hasAuthorship W4293493780A5010596687 @default.
• W4293493780 hasAuthorship W4293493780A5063285358 @default.
• W4293493780 hasConcept C109007969 @default.
• W4293493780 hasConcept C114793014 @default.
• W4293493780 hasConcept C116637073 @default.
• W4293493780 hasConcept C126559015 @default.
• W4293493780 hasConcept C127313418 @default.
• W4293493780 hasConcept C127413603 @default.
• W4293493780 hasConcept C149465734 @default.
• W4293493780 hasConcept C151730666 @default.
• W4293493780 hasConcept C153127940 @default.
• W4293493780 hasConcept C17409809 @default.
• W4293493780 hasConcept C25197100 @default.
• W4293493780 hasConcept C2778887201 @default.
• W4293493780 hasConcept C2993562611 @default.
• W4293493780 hasConcept C5900021 @default.
• W4293493780 hasConcept C78519656 @default.
• W4293493780 hasConcept C78762247 @default.
• W4293493780 hasConceptScore W4293493780C109007969 @default.
• W4293493780 hasConceptScore W4293493780C114793014 @default.
• W4293493780 hasConceptScore W4293493780C116637073 @default.
• W4293493780 hasConceptScore W4293493780C126559015 @default.
• W4293493780 hasConceptScore W4293493780C127313418 @default.
• W4293493780 hasConceptScore W4293493780C127413603 @default.
• W4293493780 hasConceptScore W4293493780C149465734 @default.
• W4293493780 hasConceptScore W4293493780C151730666 @default.
• W4293493780 hasConceptScore W4293493780C153127940 @default.
• W4293493780 hasConceptScore W4293493780C17409809 @default.
• W4293493780 hasConceptScore W4293493780C25197100 @default.
• W4293493780 hasConceptScore W4293493780C2778887201 @default.
• W4293493780 hasConceptScore W4293493780C2993562611 @default.
• W4293493780 hasConceptScore W4293493780C5900021 @default.
• W4293493780 hasConceptScore W4293493780C78519656 @default.
• W4293493780 hasConceptScore W4293493780C78762247 @default.
• W4293493780 hasFunder F4320321001 @default.
• W4293493780 hasIssue "18" @default.
• W4293493780 hasLocation W42934937801 @default.
• W4293493780 hasOpenAccess W4293493780 @default.
• W4293493780 hasPrimaryLocation W42934937801 @default.
• W4293493780 hasRelatedWork W2134197001 @default.
• W4293493780 hasRelatedWork W2243730605 @default.
• W4293493780 hasRelatedWork W2381361313 @default.
• W4293493780 hasRelatedWork W2383321979 @default.
• W4293493780 hasRelatedWork W2566858405 @default.
• W4293493780 hasRelatedWork W2937861989 @default.
• W4293493780 hasRelatedWork W2963905519 @default.
• W4293493780 hasRelatedWork W3038076967 @default.
• W4293493780 hasRelatedWork W4206598421 @default.
• W4293493780 hasRelatedWork W2595535156 @default.
• W4293493780 hasVolume "36" @default.
• W4293493780 isParatext "false" @default.
• W4293493780 isRetracted "false" @default.
• W4293493780 workType "article" @default.