FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2050793536> ?p ?o ?g. }

• W2050793536 endingPage "166" @default.
• W2050793536 startingPage "153" @default.
• W2050793536 abstract "Abstract Based on structural, geochemical, sedimentological and geochronological studies, we have formulated a model for the evolution of the late Archaean Abitibi greenstone belt of the Superior Province of Canada. The southern volcanic zone (SVZ) of the belt is dominated by komatiitic to tholeiitic volcanic plateaux and large, bimodal, mafic-felsic volcanic centres. These volcanic rocks were erupted between approximately 2710 Ma and 2700 Ma in a series of rift basins formed as a result of wrench-fault tectonics. The SVZ superimposes an older volcanic terrane which is characterized in the northern volcanic zone (NVZ) of the Abitibi belt and is approximately 2720 Ma or older. The NVZ comprises basaltic to andesitic and dacitic subaqueous massive volcanics which are cored by comagmatic sill complexes and layered mafic-anorthositic plutonic complexes. These volcanics are overlain by felsic pyroclastic rocks that were comagmatic with the emplacement of tonalitic plutons at 2717 ±2 Ma. The tectonic model envisages the SVZ to have formed in a series of rift basins which dissected an earlier formed volcanic arc (the NVZ). Analogous rift environments have been postulated for the Hokuroko basin of Japan, the Taupo volcanic zone of New Zealand and the Sumatra and Nicaragua arcs. The difference between rift related ‘submergent’ volcanism in the SVZ and ‘emergent’ volcanism in the NVZ resulted in the contrasting metallogenic styles, the former being characterized by syngenetic massive sulphide deposits, whilst the latter was dominated by epigenetic ‘porphyry-type’ Cu(Au) deposits." @default.
• W2050793536 created "2016-06-24" @default.
• W2050793536 creator A5001363940 @default.
• W2050793536 creator A5029134801 @default.
• W2050793536 creator A5082631309 @default.
• W2050793536 date "1986-03-01" @default.
• W2050793536 modified "2023-10-12" @default.
• W2050793536 title "The tectonic evolution of the Abitibi greenstone belt of Canada" @default.
• W2050793536 cites W1966256034 @default.
• W2050793536 cites W2009612684 @default.
• W2050793536 cites W2014170292 @default.
• W2050793536 cites W2017307517 @default.
• W2050793536 cites W2019582296 @default.
• W2050793536 cites W2020774528 @default.
• W2050793536 cites W2022463607 @default.
• W2050793536 cites W2030993349 @default.
• W2050793536 cites W2031407838 @default.
• W2050793536 cites W2036591421 @default.
• W2050793536 cites W2053579895 @default.
• W2050793536 cites W2054104477 @default.
• W2050793536 cites W2059359947 @default.
• W2050793536 cites W2068891498 @default.
• W2050793536 cites W2081357561 @default.
• W2050793536 cites W2085289041 @default.
• W2050793536 cites W2105910619 @default.
• W2050793536 cites W2145552866 @default.
• W2050793536 cites W2909805201 @default.
• W2050793536 cites W2909855584 @default.
• W2050793536 doi "https://doi.org/10.1017/s0016756800029800" @default.
• W2050793536 hasPublicationYear "1986" @default.
• W2050793536 type Work @default.
• W2050793536 sameAs 2050793536 @default.
• W2050793536 citedByCount "121" @default.
• W2050793536 countsByYear W20507935362012 @default.
• W2050793536 countsByYear W20507935362013 @default.
• W2050793536 countsByYear W20507935362014 @default.
• W2050793536 countsByYear W20507935362015 @default.
• W2050793536 countsByYear W20507935362016 @default.
• W2050793536 countsByYear W20507935362017 @default.
• W2050793536 countsByYear W20507935362018 @default.
• W2050793536 countsByYear W20507935362019 @default.
• W2050793536 countsByYear W20507935362020 @default.
• W2050793536 countsByYear W20507935362021 @default.
• W2050793536 countsByYear W20507935362022 @default.
• W2050793536 crossrefType "journal-article" @default.
• W2050793536 hasAuthorship W2050793536A5001363940 @default.
• W2050793536 hasAuthorship W2050793536A5029134801 @default.
• W2050793536 hasAuthorship W2050793536A5082631309 @default.
• W2050793536 hasConcept C104962623 @default.
• W2050793536 hasConcept C120806208 @default.
• W2050793536 hasConcept C127313418 @default.
• W2050793536 hasConcept C149347711 @default.
• W2050793536 hasConcept C150999391 @default.
• W2050793536 hasConcept C151730666 @default.
• W2050793536 hasConcept C161509811 @default.
• W2050793536 hasConcept C167284885 @default.
• W2050793536 hasConcept C17409809 @default.
• W2050793536 hasConcept C192241223 @default.
• W2050793536 hasConcept C193429443 @default.
• W2050793536 hasConcept C2778703903 @default.
• W2050793536 hasConcept C2780733770 @default.
• W2050793536 hasConcept C50682988 @default.
• W2050793536 hasConcept C5900021 @default.
• W2050793536 hasConcept C77928131 @default.
• W2050793536 hasConcept C95869378 @default.
• W2050793536 hasConceptScore W2050793536C104962623 @default.
• W2050793536 hasConceptScore W2050793536C120806208 @default.
• W2050793536 hasConceptScore W2050793536C127313418 @default.
• W2050793536 hasConceptScore W2050793536C149347711 @default.
• W2050793536 hasConceptScore W2050793536C150999391 @default.
• W2050793536 hasConceptScore W2050793536C151730666 @default.
• W2050793536 hasConceptScore W2050793536C161509811 @default.
• W2050793536 hasConceptScore W2050793536C167284885 @default.
• W2050793536 hasConceptScore W2050793536C17409809 @default.
• W2050793536 hasConceptScore W2050793536C192241223 @default.
• W2050793536 hasConceptScore W2050793536C193429443 @default.
• W2050793536 hasConceptScore W2050793536C2778703903 @default.
• W2050793536 hasConceptScore W2050793536C2780733770 @default.
• W2050793536 hasConceptScore W2050793536C50682988 @default.
• W2050793536 hasConceptScore W2050793536C5900021 @default.
• W2050793536 hasConceptScore W2050793536C77928131 @default.
• W2050793536 hasConceptScore W2050793536C95869378 @default.
• W2050793536 hasIssue "2" @default.
• W2050793536 hasLocation W20507935361 @default.
• W2050793536 hasOpenAccess W2050793536 @default.
• W2050793536 hasPrimaryLocation W20507935361 @default.
• W2050793536 hasRelatedWork W2009520377 @default.
• W2050793536 hasRelatedWork W2020860341 @default.
• W2050793536 hasRelatedWork W2023774480 @default.
• W2050793536 hasRelatedWork W2037553978 @default.
• W2050793536 hasRelatedWork W2047673727 @default.
• W2050793536 hasRelatedWork W2050793536 @default.
• W2050793536 hasRelatedWork W2051175737 @default.
• W2050793536 hasRelatedWork W2055445924 @default.
• W2050793536 hasRelatedWork W2079702919 @default.
• W2050793536 hasRelatedWork W2948384908 @default.
• W2050793536 hasVolume "123" @default.
• W2050793536 isParatext "false" @default.

• next