FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2018926695> ?p ?o ?g. }

• W2018926695 endingPage "75" @default.
• W2018926695 startingPage "61" @default.
• W2018926695 abstract "Abstract A major cluster of anorogenic A-type, subvolcanic ring complexes of Silurian to Jurassic age is emplaced into Proterozoic rocks of the basement complex in the Bayuda Desert of northern Sudan. The complexes belong to the Younger granite association which is widespread throughout the Sudan and environs. The Ras ed Dom complex is a striking example of migrating centres in which intrusive activity shifted eastwards and declined in strength with time. Intrusive rocks predominate and consist of metaluminous and peralkaline syenites and granites. Field relations indicate that the sequence metaluminous syenite-peralkaline syenite-peralkaline granite is a recurrent fractionation series representing high level fractionation of a parental metaluminous syeno-monzonitic magma. The metaluminous syenites contain rare early-formed plagioclase (oligoclase-andesine) but otherwise the suite is typically hypersolvus. The metaluminous rocks are characterised by an early pyroxene zone from ferrohedenbergite to aegirine-augite and enclosed in ferroedenitic amphibole. Microprobe analysis reveals a broad range of amphibole compositions in the peralkaline rocks, comprising ferrorichterite-arfvedsonite-riebeckite solid solutions. Late aegirine, exhibiting marked enrichment in the acmite component, typically replaces the arfvedsonite, especially in the granites. Extremely pure albite accompanies aegirine and the development of these phases is attributed to limited interaction between the rocks and late sodic fluids. Geochemical variation in the suite includes marked depletions of CaO, Ba and Sr with increasing silica, consistent with fractionational removal of alkali-feldspar. The peralkalinity of the later rocks has been enhanced by sodic autometasomatism, reflected in their high contents of REE and HFS elements such as Zr, Nb and Ga, and by the erratic distribution of these elements. LREE-enrichment in the suite is marked and suggests equilibrium with a residual HREE-rich phase such as garnet in the source rocks. The Younger Granite magmas are attributed to melting of a lower crustal mafic-rich source such as garnet-eclogite. The heat for this anatectic event is thought to have come from mantle-derived basalt magma, the uprise of which was largely checked in the lower crust, only minor amounts reaching the surface." @default.
• W2018926695 created "2016-06-24" @default.
• W2018926695 creator A5090276844 @default.
• W2018926695 date "1985-01-01" @default.
• W2018926695 modified "2023-09-26" @default.
• W2018926695 title "Ras ed Dom migrating ring complex: A-type granites and syenites from the Bayuda Desert, Sudan" @default.
• W2018926695 cites W1671578975 @default.
• W2018926695 cites W1977711933 @default.
• W2018926695 cites W1981626109 @default.
• W2018926695 cites W1990501577 @default.
• W2018926695 cites W1992510801 @default.
• W2018926695 cites W1998861973 @default.
• W2018926695 cites W2004330320 @default.
• W2018926695 cites W2005151756 @default.
• W2018926695 cites W2006254591 @default.
• W2018926695 cites W2009520093 @default.
• W2018926695 cites W2016669290 @default.
• W2018926695 cites W2031295074 @default.
• W2018926695 cites W2031645706 @default.
• W2018926695 cites W2037588390 @default.
• W2018926695 cites W2042803182 @default.
• W2018926695 cites W2052055789 @default.
• W2018926695 cites W2060683566 @default.
• W2018926695 cites W2061162406 @default.
• W2018926695 cites W2064226583 @default.
• W2018926695 cites W2070208280 @default.
• W2018926695 cites W2075517248 @default.
• W2018926695 cites W2077418438 @default.
• W2018926695 cites W2079918042 @default.
• W2018926695 cites W2084976632 @default.
• W2018926695 cites W2089674622 @default.
• W2018926695 cites W2091628246 @default.
• W2018926695 cites W2105938399 @default.
• W2018926695 cites W2112333790 @default.
• W2018926695 cites W2118300487 @default.
• W2018926695 cites W2312666490 @default.
• W2018926695 cites W2329112687 @default.
• W2018926695 cites W2329456392 @default.
• W2018926695 cites W2330773227 @default.
• W2018926695 cites W2331272198 @default.
• W2018926695 cites W2331350605 @default.
• W2018926695 cites W2889900102 @default.
• W2018926695 cites W4243291828 @default.
• W2018926695 doi "https://doi.org/10.1016/0899-5362(85)90023-5" @default.
• W2018926695 hasPublicationYear "1985" @default.
• W2018926695 type Work @default.
• W2018926695 sameAs 2018926695 @default.
• W2018926695 citedByCount "20" @default.
• W2018926695 countsByYear W20189266952013 @default.
• W2018926695 countsByYear W20189266952014 @default.
• W2018926695 countsByYear W20189266952017 @default.
• W2018926695 countsByYear W20189266952018 @default.
• W2018926695 countsByYear W20189266952019 @default.
• W2018926695 countsByYear W20189266952020 @default.
• W2018926695 countsByYear W20189266952022 @default.
• W2018926695 crossrefType "journal-article" @default.
• W2018926695 hasAuthorship W2018926695A5090276844 @default.
• W2018926695 hasConcept C127313418 @default.
• W2018926695 hasConcept C151730666 @default.
• W2018926695 hasConcept C166957645 @default.
• W2018926695 hasConcept C17409809 @default.
• W2018926695 hasConcept C17744445 @default.
• W2018926695 hasConcept C178790620 @default.
• W2018926695 hasConcept C185592680 @default.
• W2018926695 hasConcept C199539241 @default.
• W2018926695 hasConcept C205649164 @default.
• W2018926695 hasConcept C2776130869 @default.
• W2018926695 hasConcept C2777299769 @default.
• W2018926695 hasConcept C2780378348 @default.
• W2018926695 hasConceptScore W2018926695C127313418 @default.
• W2018926695 hasConceptScore W2018926695C151730666 @default.
• W2018926695 hasConceptScore W2018926695C166957645 @default.
• W2018926695 hasConceptScore W2018926695C17409809 @default.
• W2018926695 hasConceptScore W2018926695C17744445 @default.
• W2018926695 hasConceptScore W2018926695C178790620 @default.
• W2018926695 hasConceptScore W2018926695C185592680 @default.
• W2018926695 hasConceptScore W2018926695C199539241 @default.
• W2018926695 hasConceptScore W2018926695C205649164 @default.
• W2018926695 hasConceptScore W2018926695C2776130869 @default.
• W2018926695 hasConceptScore W2018926695C2777299769 @default.
• W2018926695 hasConceptScore W2018926695C2780378348 @default.
• W2018926695 hasIssue "1-2" @default.
• W2018926695 hasLocation W20189266951 @default.
• W2018926695 hasOpenAccess W2018926695 @default.
• W2018926695 hasPrimaryLocation W20189266951 @default.
• W2018926695 hasRelatedWork W1758497512 @default.
• W2018926695 hasRelatedWork W1987691177 @default.
• W2018926695 hasRelatedWork W2036099453 @default.
• W2018926695 hasRelatedWork W2040829098 @default.
• W2018926695 hasRelatedWork W2349947565 @default.
• W2018926695 hasRelatedWork W2361911732 @default.
• W2018926695 hasRelatedWork W2380934447 @default.
• W2018926695 hasRelatedWork W2538103680 @default.
• W2018926695 hasRelatedWork W2748952813 @default.
• W2018926695 hasRelatedWork W4380204653 @default.
• W2018926695 hasVolume "3" @default.
• W2018926695 isParatext "false" @default.
• W2018926695 isRetracted "false" @default.

• next