FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023168726> ?p ?o ?g. }

• W2023168726 endingPage "138" @default.
• W2023168726 startingPage "125" @default.
• W2023168726 abstract "The single zircon evaporation, SHRIMP ion-microprobe and conventional dissolution techniques were used to determine 207Pb/206Pb and UPb ages on samples from the Upper Onverwacht and Fig Tree groups of the early Archean Barberton greenstone belt, South Africa. Zircons from dacitic rocks of the upper Hooggenoeg Formation yield ages of ∼ 3445–3452 Ma. A tuff in the basal Kromberg Formation has a mean age of 3416 ± 5 Ma. A tuffaceous band, 5 cm thick, in the uppermost Kromberg Formation contains igneous zircons with a mean age of 3334 ± 3 Ma. The 1700 m section of Kromberg Formation between these two samples is composed of basaltic lavas, minor komatiites and cherty metasediments. The overlying Mendon Formation is composed of interbedded komatiitic lavas and metasediments with a minimum thickness of 600 m. A cherty, stromatolitic metasediment 300 m above the base contains several thin ash layers with a mean zircon age of 3298 ± 3 Ma. The basal Fig Tree Group has units as old as 3259 ± 3 Ma, and upper units in the Fig Tree are as young as 3225 ± 3 Ma. Xenocrystic zircons in the Upper Onverwacht and overlying Fig Tree Group samples suggest that successive igneous units inherited zircons from underlying units and that, over several hundred million years, episodes of intermediate to felsic igneous activity took place at 20–40 Ma intervals. Structural repetition by isoclinal folding and thrust faulting are important components of late greenstone belt evolution, but should not obscure the importance of the prolonged interval of magmatic evolution represented by the thick pile of volcanic rocks observed in the Barberton greenstone belt." @default.
• W2023168726 created "2016-06-24" @default.
• W2023168726 creator A5006591356 @default.
• W2023168726 creator A5015701979 @default.
• W2023168726 creator A5019581661 @default.
• W2023168726 creator A5062407746 @default.
• W2023168726 creator A5069826985 @default.
• W2023168726 date "1996-05-01" @default.
• W2023168726 modified "2023-10-13" @default.
• W2023168726 title "Prolonged magmatism and time constraints for sediment deposition in the early Archean Barberton greenstone belt: evidence from the Upper Onverwacht and Fig Tree groups" @default.
• W2023168726 cites W1965960661 @default.
• W2023168726 cites W1967532698 @default.
• W2023168726 cites W1967589404 @default.
• W2023168726 cites W1969846781 @default.
• W2023168726 cites W1983818767 @default.
• W2023168726 cites W1984007664 @default.
• W2023168726 cites W1999185112 @default.
• W2023168726 cites W2011763496 @default.
• W2023168726 cites W2011848554 @default.
• W2023168726 cites W2011909094 @default.
• W2023168726 cites W2015204472 @default.
• W2023168726 cites W2018245819 @default.
• W2023168726 cites W2021398206 @default.
• W2023168726 cites W2022236881 @default.
• W2023168726 cites W2040223134 @default.
• W2023168726 cites W2042491470 @default.
• W2023168726 cites W2044114056 @default.
• W2023168726 cites W2050139372 @default.
• W2023168726 cites W2050426306 @default.
• W2023168726 cites W2057208829 @default.
• W2023168726 cites W2072176226 @default.
• W2023168726 cites W2077783204 @default.
• W2023168726 cites W2084107243 @default.
• W2023168726 cites W2089351169 @default.
• W2023168726 cites W2097625820 @default.
• W2023168726 cites W2114276383 @default.
• W2023168726 cites W2139851035 @default.
• W2023168726 cites W2144457675 @default.
• W2023168726 cites W2152428293 @default.
• W2023168726 cites W2155512758 @default.
• W2023168726 cites W2158061484 @default.
• W2023168726 cites W2163006245 @default.
• W2023168726 cites W2317096966 @default.
• W2023168726 doi "https://doi.org/10.1016/0301-9268(95)00073-9" @default.
• W2023168726 hasPublicationYear "1996" @default.
• W2023168726 type Work @default.
• W2023168726 sameAs 2023168726 @default.
• W2023168726 citedByCount "204" @default.
• W2023168726 countsByYear W20231687262012 @default.
• W2023168726 countsByYear W20231687262013 @default.
• W2023168726 countsByYear W20231687262014 @default.
• W2023168726 countsByYear W20231687262015 @default.
• W2023168726 countsByYear W20231687262016 @default.
• W2023168726 countsByYear W20231687262017 @default.
• W2023168726 countsByYear W20231687262018 @default.
• W2023168726 countsByYear W20231687262019 @default.
• W2023168726 countsByYear W20231687262020 @default.
• W2023168726 countsByYear W20231687262021 @default.
• W2023168726 countsByYear W20231687262022 @default.
• W2023168726 countsByYear W20231687262023 @default.
• W2023168726 crossrefType "journal-article" @default.
• W2023168726 hasAuthorship W2023168726A5006591356 @default.
• W2023168726 hasAuthorship W2023168726A5015701979 @default.
• W2023168726 hasAuthorship W2023168726A5019581661 @default.
• W2023168726 hasAuthorship W2023168726A5062407746 @default.
• W2023168726 hasAuthorship W2023168726A5069826985 @default.
• W2023168726 hasConcept C127313418 @default.
• W2023168726 hasConcept C149347711 @default.
• W2023168726 hasConcept C161509811 @default.
• W2023168726 hasConcept C167284885 @default.
• W2023168726 hasConcept C173776410 @default.
• W2023168726 hasConcept C17409809 @default.
• W2023168726 hasConcept C193429443 @default.
• W2023168726 hasConcept C195081551 @default.
• W2023168726 hasConcept C2778849375 @default.
• W2023168726 hasConcept C2780733770 @default.
• W2023168726 hasConcept C42787717 @default.
• W2023168726 hasConceptScore W2023168726C127313418 @default.
• W2023168726 hasConceptScore W2023168726C149347711 @default.
• W2023168726 hasConceptScore W2023168726C161509811 @default.
• W2023168726 hasConceptScore W2023168726C167284885 @default.
• W2023168726 hasConceptScore W2023168726C173776410 @default.
• W2023168726 hasConceptScore W2023168726C17409809 @default.
• W2023168726 hasConceptScore W2023168726C193429443 @default.
• W2023168726 hasConceptScore W2023168726C195081551 @default.
• W2023168726 hasConceptScore W2023168726C2778849375 @default.
• W2023168726 hasConceptScore W2023168726C2780733770 @default.
• W2023168726 hasConceptScore W2023168726C42787717 @default.
• W2023168726 hasIssue "1-3" @default.
• W2023168726 hasLocation W20231687261 @default.
• W2023168726 hasOpenAccess W2023168726 @default.
• W2023168726 hasPrimaryLocation W20231687261 @default.
• W2023168726 hasRelatedWork W1971994039 @default.
• W2023168726 hasRelatedWork W2015115766 @default.
• W2023168726 hasRelatedWork W2016799189 @default.
• W2023168726 hasRelatedWork W2076563219 @default.
• W2023168726 hasRelatedWork W2081032602 @default.
• W2023168726 hasRelatedWork W2090312536 @default.

• next