FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2127145395> ?p ?o ?g. }

• W2127145395 endingPage "248" @default.
• W2127145395 startingPage "219" @default.
• W2127145395 abstract "Detailed mapping, structural analysis and high precision UPb zircon ages from hypabyssal porphyries and tonalites has enabled the timing of the major collisional episode of the Barberton greenstone belt to be determined. This episode, known as the D2 deformation, can be divided into D2-early and D2-late. D2-early deformation, bracketed as having occurred between 3229 and 3227 Ma, was typified by isoclinal folding (F2 of shales and associated cherts (Fig Tree Group), but not of the overlying quartzose clastic rocks (Moodies Group). D2-late deformation was at 3226 Ma, or later, with large F3 open-tight folds dominating the map pattern in the Weltevreden study area. Late D2 faults, such as the Moodies Fault, that define the boundaries of the major structural domains converge near the Saddleback Fault, a major boundary within the Barberton greenstone belt. Strain calculations suggest that plane strain was dominant, with at least 60% shortening occurring during the D2 deformational events. Although an early and a late stage of D2 deformation can be distinguished in the field, precise UPb zircon ages indicate that these events represent a continuum, ranging from the onset of an arc-arc assembly event (D2-early), through to major collisional and post-amalgamation events (D2-late), all of which spanned ∼3 million years. La cartographie détailĺee, l'analyse structurale et la datation de haute précision UPb sur zircon dans les porphyres subvolcaniques et les tonalites a permis de déterminer la durée de l'épisode majeur de collision dans la ceinture des roches vertes de Barberton. Cetépisode, connu sous le nom de déformation D2, peut se subdiviser en D2-précoce et D2-tardif. La déformation D2-précoce, dont la fourchette d'aˆges se situe entre 3229 et 3227 Ma, est caractérisée typiquement par le plissement isoclinal F2 des shales et des cherts associés du Groupe de Fig Tree, et non des roches clastiques quartzeuses susjacentes du Groupe de Moodies. La déformation D2-tardive s'est produite il y a 3226 Ma, ou plus tard, avec de grands plis ouvertsàfermés F3 responsables de la structure générale visible sur la carte de la zone d'étude de Weltevreden. Les failles D2-tardives, comme la Faille de Moodies, définissent les limites des grands domaines structuraux et convergent près de la Faille de Saddleback, limite majeureàl'intérieur de la ceinture de roches vertes de Barberton. Le calcul des déformations suggère une déformation plane dominante, avec au moins 60% de raccourcissement durant lesépisodes de déformation D2. Bien que l'on puisse distinguer sur le terrain un stage precoce et un stage tardif de la deformation D2, lesaˆges précis UPb sur zircon indiquent que cesévénements représentent un continuumàpartir du début de l'assemblage arc-arc (D2-précoce) jusqu'àla collision majeure et le stage post-collage (D2-tardif), le tout durant environ 3 millions d'années." @default.
• W2127145395 created "2016-06-24" @default.
• W2127145395 creator A5055848554 @default.
• W2127145395 creator A5060490525 @default.
• W2127145395 date "2000-02-01" @default.
• W2127145395 modified "2023-10-04" @default.
• W2127145395 title "An Arch˦an arc-arc collisional event: a short-lived (ca 3 Myr) episode, Weltevreden area, Barberton greenstone belt, South Africa" @default.
• W2127145395 cites W1964778916 @default.
• W2127145395 cites W1965858395 @default.
• W2127145395 cites W1965960661 @default.
• W2127145395 cites W1966256034 @default.
• W2127145395 cites W1969846781 @default.
• W2127145395 cites W1971836134 @default.
• W2127145395 cites W1977630723 @default.
• W2127145395 cites W1978916926 @default.
• W2127145395 cites W1979771017 @default.
• W2127145395 cites W1993271872 @default.
• W2127145395 cites W1999185112 @default.
• W2127145395 cites W2000599635 @default.
• W2127145395 cites W2002719347 @default.
• W2127145395 cites W2007105153 @default.
• W2127145395 cites W2009962074 @default.
• W2127145395 cites W2024954226 @default.
• W2127145395 cites W2028866306 @default.
• W2127145395 cites W2032366241 @default.
• W2127145395 cites W2032929243 @default.
• W2127145395 cites W2033988074 @default.
• W2127145395 cites W2035674133 @default.
• W2127145395 cites W2040223134 @default.
• W2127145395 cites W2042582115 @default.
• W2127145395 cites W2045928812 @default.
• W2127145395 cites W2048568469 @default.
• W2127145395 cites W2048945399 @default.
• W2127145395 cites W2050139372 @default.
• W2127145395 cites W2050426306 @default.
• W2127145395 cites W2050629319 @default.
• W2127145395 cites W2055525892 @default.
• W2127145395 cites W2059946437 @default.
• W2127145395 cites W2060439713 @default.
• W2127145395 cites W2072130111 @default.
• W2127145395 cites W2082241110 @default.
• W2127145395 cites W2083774164 @default.
• W2127145395 cites W2084107243 @default.
• W2127145395 cites W2086859942 @default.
• W2127145395 cites W2089351169 @default.
• W2127145395 cites W2095448843 @default.
• W2127145395 cites W2097625820 @default.
• W2127145395 cites W2129751985 @default.
• W2127145395 cites W2153161505 @default.
• W2127145395 doi "https://doi.org/10.1016/s0899-5362(00)00017-8" @default.
• W2127145395 hasPublicationYear "2000" @default.
• W2127145395 type Work @default.
• W2127145395 sameAs 2127145395 @default.
• W2127145395 citedByCount "92" @default.
• W2127145395 countsByYear W21271453952012 @default.
• W2127145395 countsByYear W21271453952013 @default.
• W2127145395 countsByYear W21271453952014 @default.
• W2127145395 countsByYear W21271453952015 @default.
• W2127145395 countsByYear W21271453952016 @default.
• W2127145395 countsByYear W21271453952017 @default.
• W2127145395 countsByYear W21271453952018 @default.
• W2127145395 countsByYear W21271453952019 @default.
• W2127145395 countsByYear W21271453952020 @default.
• W2127145395 countsByYear W21271453952021 @default.
• W2127145395 countsByYear W21271453952022 @default.
• W2127145395 countsByYear W21271453952023 @default.
• W2127145395 crossrefType "journal-article" @default.
• W2127145395 hasAuthorship W2127145395A5055848554 @default.
• W2127145395 hasAuthorship W2127145395A5060490525 @default.
• W2127145395 hasConcept C127313418 @default.
• W2127145395 hasConcept C149347711 @default.
• W2127145395 hasConcept C150999391 @default.
• W2127145395 hasConcept C151730666 @default.
• W2127145395 hasConcept C165205528 @default.
• W2127145395 hasConcept C17409809 @default.
• W2127145395 hasConcept C2778849375 @default.
• W2127145395 hasConcept C2780733770 @default.
• W2127145395 hasConcept C77928131 @default.
• W2127145395 hasConceptScore W2127145395C127313418 @default.
• W2127145395 hasConceptScore W2127145395C149347711 @default.
• W2127145395 hasConceptScore W2127145395C150999391 @default.
• W2127145395 hasConceptScore W2127145395C151730666 @default.
• W2127145395 hasConceptScore W2127145395C165205528 @default.
• W2127145395 hasConceptScore W2127145395C17409809 @default.
• W2127145395 hasConceptScore W2127145395C2778849375 @default.
• W2127145395 hasConceptScore W2127145395C2780733770 @default.
• W2127145395 hasConceptScore W2127145395C77928131 @default.
• W2127145395 hasIssue "2" @default.
• W2127145395 hasLocation W21271453951 @default.
• W2127145395 hasOpenAccess W2127145395 @default.
• W2127145395 hasPrimaryLocation W21271453951 @default.
• W2127145395 hasRelatedWork W1499470380 @default.
• W2127145395 hasRelatedWork W1602785432 @default.
• W2127145395 hasRelatedWork W2057167278 @default.
• W2127145395 hasRelatedWork W2060155879 @default.
• W2127145395 hasRelatedWork W2069683510 @default.
• W2127145395 hasRelatedWork W2604731307 @default.
• W2127145395 hasRelatedWork W2743919463 @default.

• next