Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897310878> ?p ?o ?g. }
- W2897310878 endingPage "291" @default.
- W2897310878 startingPage "282" @default.
- W2897310878 abstract "To reveal the characteristics of fractures in high quality shale reservoir and to find regions that are favorable for shale gas accumulation, the characteristics of fractures and their effect on the shale gas content in the lower Cambrian marine shale from 2 typical shale gas wells in the Upper Yangtze have been analyzed in detail by observing the shale cores, scanning electron microscope photographs and rock slice pictures associated with various geochemical data. Five types of macrofractures (high-angle shearing fracture, tension-shearing fracture, compresso-shearing fracture, low-angle slip fracture, and bedding fracture) and 4 types of microfractures (interlayer fracture, inter-particle fracture, intra-particle fracture, and organic matter-associated fracture) have been identified in the lower Cambrian shale. The fractures in lower Cambrian shale have 5 possible origins: 1 generated by tectonic tension and shearing stresses; 2 cracking due to loading pressure relief; 3 corroded by acidic fluids during hydrocarbon generation; 4 induced by overpressured fluid; 5 formed due to diagenesis-associated shrinkage of mineral crystals. In general, the shale in Sichuan Basin contains more nonstructural fractures (including bedding fractures and microfractures), whereas shale outside the basin contains more structural fractures (including high-angle shearing fractures, tension-shearing fractures, and low-angle slip fractures). Three controlling factors of fracture development be summarized as follows: 1 tectonic setting; 2 mineral components; 3 organic matter content and maturity. In conclusion, structural fractures can be considered as destructive, and nonstructural fractures can be considered as favorable. Shale gas reservoirs can be divided into 3 types: type A with a shale gas content >2 m3/t, destructive/structural fractures <20/m, and favorable/nonstructural fractures >100/m; type B with a shale gas content of 1 m3/t - 2 m3/t, destructive/structural fractures <20/m, and favorable/nonstructural fractures 50/m −100/m; (3) type C with a shale gas content < 1 m3/t, destructive/structural fractures >20/m, or destructive/structural fractures <20/m, and favorable/nonstructural fractures <50/m." @default.
- W2897310878 created "2018-10-26" @default.
- W2897310878 creator A5001163607 @default.
- W2897310878 creator A5017810268 @default.
- W2897310878 creator A5030362872 @default.
- W2897310878 creator A5034396097 @default.
- W2897310878 creator A5039410252 @default.
- W2897310878 creator A5042192229 @default.
- W2897310878 creator A5070551517 @default.
- W2897310878 date "2019-01-01" @default.
- W2897310878 modified "2023-10-08" @default.
- W2897310878 title "Fracture types in the lower Cambrian shale and their effect on shale gas accumulation, Upper Yangtze" @default.
- W2897310878 cites W1967390332 @default.
- W2897310878 cites W1979044833 @default.
- W2897310878 cites W1995026965 @default.
- W2897310878 cites W1997666964 @default.
- W2897310878 cites W2022888492 @default.
- W2897310878 cites W2058001179 @default.
- W2897310878 cites W2071771565 @default.
- W2897310878 cites W2090307063 @default.
- W2897310878 cites W2091691832 @default.
- W2897310878 cites W2101691304 @default.
- W2897310878 cites W2123178635 @default.
- W2897310878 cites W2126624631 @default.
- W2897310878 cites W2150922969 @default.
- W2897310878 cites W2156037206 @default.
- W2897310878 cites W2161051067 @default.
- W2897310878 cites W2163236950 @default.
- W2897310878 cites W2166476646 @default.
- W2897310878 cites W2170995602 @default.
- W2897310878 cites W2326312167 @default.
- W2897310878 cites W2521407017 @default.
- W2897310878 cites W2787874873 @default.
- W2897310878 cites W292821781 @default.
- W2897310878 doi "https://doi.org/10.1016/j.marpetgeo.2018.10.030" @default.
- W2897310878 hasPublicationYear "2019" @default.
- W2897310878 type Work @default.
- W2897310878 sameAs 2897310878 @default.
- W2897310878 citedByCount "33" @default.
- W2897310878 countsByYear W28973108782019 @default.
- W2897310878 countsByYear W28973108782020 @default.
- W2897310878 countsByYear W28973108782021 @default.
- W2897310878 countsByYear W28973108782022 @default.
- W2897310878 countsByYear W28973108782023 @default.
- W2897310878 crossrefType "journal-article" @default.
- W2897310878 hasAuthorship W2897310878A5001163607 @default.
- W2897310878 hasAuthorship W2897310878A5017810268 @default.
- W2897310878 hasAuthorship W2897310878A5030362872 @default.
- W2897310878 hasAuthorship W2897310878A5034396097 @default.
- W2897310878 hasAuthorship W2897310878A5039410252 @default.
- W2897310878 hasAuthorship W2897310878A5042192229 @default.
- W2897310878 hasAuthorship W2897310878A5070551517 @default.
- W2897310878 hasConcept C127313418 @default.
- W2897310878 hasConcept C127413603 @default.
- W2897310878 hasConcept C130452526 @default.
- W2897310878 hasConcept C144027150 @default.
- W2897310878 hasConcept C151730666 @default.
- W2897310878 hasConcept C152279782 @default.
- W2897310878 hasConcept C153127940 @default.
- W2897310878 hasConcept C17409809 @default.
- W2897310878 hasConcept C187320778 @default.
- W2897310878 hasConcept C2777232088 @default.
- W2897310878 hasConcept C43369102 @default.
- W2897310878 hasConcept C518851703 @default.
- W2897310878 hasConcept C548081761 @default.
- W2897310878 hasConcept C5900021 @default.
- W2897310878 hasConcept C86803240 @default.
- W2897310878 hasConceptScore W2897310878C127313418 @default.
- W2897310878 hasConceptScore W2897310878C127413603 @default.
- W2897310878 hasConceptScore W2897310878C130452526 @default.
- W2897310878 hasConceptScore W2897310878C144027150 @default.
- W2897310878 hasConceptScore W2897310878C151730666 @default.
- W2897310878 hasConceptScore W2897310878C152279782 @default.
- W2897310878 hasConceptScore W2897310878C153127940 @default.
- W2897310878 hasConceptScore W2897310878C17409809 @default.
- W2897310878 hasConceptScore W2897310878C187320778 @default.
- W2897310878 hasConceptScore W2897310878C2777232088 @default.
- W2897310878 hasConceptScore W2897310878C43369102 @default.
- W2897310878 hasConceptScore W2897310878C518851703 @default.
- W2897310878 hasConceptScore W2897310878C548081761 @default.
- W2897310878 hasConceptScore W2897310878C5900021 @default.
- W2897310878 hasConceptScore W2897310878C86803240 @default.
- W2897310878 hasFunder F4320321543 @default.
- W2897310878 hasLocation W28973108781 @default.
- W2897310878 hasOpenAccess W2897310878 @default.
- W2897310878 hasPrimaryLocation W28973108781 @default.
- W2897310878 hasRelatedWork W1975729326 @default.
- W2897310878 hasRelatedWork W1987965304 @default.
- W2897310878 hasRelatedWork W1994348428 @default.
- W2897310878 hasRelatedWork W2324542482 @default.
- W2897310878 hasRelatedWork W2356329742 @default.
- W2897310878 hasRelatedWork W2594306655 @default.
- W2897310878 hasRelatedWork W4214563068 @default.
- W2897310878 hasRelatedWork W4252288145 @default.
- W2897310878 hasRelatedWork W4368374958 @default.
- W2897310878 hasRelatedWork W2201233961 @default.
- W2897310878 hasVolume "99" @default.
- W2897310878 isParatext "false" @default.