FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014997629> ?p ?o ?g. }

• W2014997629 endingPage "145" @default.
• W2014997629 startingPage "129" @default.
• W2014997629 abstract "New field work, in addition to zircon geochronology, Nd isotopes and reconnaissance geochemical data allow the recognition of Paleoproterozoic volcanic and metavolcanic sequences in the São Luís Craton of northern Brazil. These sequences record at least five volcanic pulses occurring probably in three distinct epochs and in different tectonic settings. (1) The Pirocaua Formation of the Aurizona Group comprises early arc-related calc-alkaline metapyroclastic rocks of 2240 ± 5 Ma formed from juvenile protoliths in addition to minor older crustal components. (2) The Matará Formation of the Aurizona Group holds mafic tholeiitic and ultramafic metavolcanic rocks of back arc and/or island arc setting, which are likely coeval to the Pirocaua Formation. (3) The Serra do Jacaré volcanic unit is composed of tholeiitic basalts and predominantly metaluminous, normal- to high-K calc-alkaline andesites of 2164 ± 3 Ma formed in mature arc or active continental margin from juvenile protoliths along with subordinate older (Paleoproterozoic) materials and associated to the main calc-alkaline orogenic stage. (4) The Rio Diamante Formation consists of late-orogenic metaluminous, medium-K, calc-alkaline rhyolite to dacite and tuffs of 2160 ± 8 Ma formed in continental margin setting from reworked Paleoproterozoic crust (island arc) with incipient Archean contribution. (5) The Rosilha volcanic unit is composed of weakly peraluminous, medium-K, calc-alkaline dacite and tuff formed probably at about 2068 Ma from reworked crustal protoliths. As a whole the volcanic and metavolcanic rocks record and characterized better the previously proposed orogenic evolution of the São Luís Craton." @default.
• W2014997629 created "2016-06-24" @default.
• W2014997629 creator A5003977888 @default.
• W2014997629 creator A5008860230 @default.
• W2014997629 creator A5022116081 @default.
• W2014997629 creator A5027405014 @default.
• W2014997629 creator A5034267164 @default.
• W2014997629 creator A5043884920 @default.
• W2014997629 date "2009-02-01" @default.
• W2014997629 modified "2023-10-06" @default.
• W2014997629 title "Geochronology, Nd isotopes and reconnaissance geochemistry of volcanic and metavolcanic rocks of the São Luís Craton, northern Brazil: Implications for tectonic setting and crustal evolution" @default.
• W2014997629 cites W1976384188 @default.
• W2014997629 cites W1987013508 @default.
• W2014997629 cites W1992364224 @default.
• W2014997629 cites W1996377397 @default.
• W2014997629 cites W1999448338 @default.
• W2014997629 cites W2004458753 @default.
• W2014997629 cites W2007105153 @default.
• W2014997629 cites W2012718531 @default.
• W2014997629 cites W2015860455 @default.
• W2014997629 cites W2031791685 @default.
• W2014997629 cites W2044114056 @default.
• W2014997629 cites W2049568230 @default.
• W2014997629 cites W2057208829 @default.
• W2014997629 cites W2090781688 @default.
• W2014997629 cites W2098442602 @default.
• W2014997629 cites W2098605918 @default.
• W2014997629 cites W2105308503 @default.
• W2014997629 cites W2108971421 @default.
• W2014997629 cites W2112435406 @default.
• W2014997629 cites W2141946675 @default.
• W2014997629 cites W2144355237 @default.
• W2014997629 cites W2151802570 @default.
• W2014997629 cites W2159082531 @default.
• W2014997629 cites W2916760013 @default.
• W2014997629 doi "https://doi.org/10.1016/j.jsames.2008.07.001" @default.
• W2014997629 hasPublicationYear "2009" @default.
• W2014997629 type Work @default.
• W2014997629 sameAs 2014997629 @default.
• W2014997629 citedByCount "17" @default.
• W2014997629 countsByYear W20149976292012 @default.
• W2014997629 countsByYear W20149976292013 @default.
• W2014997629 countsByYear W20149976292014 @default.
• W2014997629 countsByYear W20149976292015 @default.
• W2014997629 countsByYear W20149976292016 @default.
• W2014997629 countsByYear W20149976292017 @default.
• W2014997629 countsByYear W20149976292018 @default.
• W2014997629 countsByYear W20149976292019 @default.
• W2014997629 countsByYear W20149976292020 @default.
• W2014997629 countsByYear W20149976292022 @default.
• W2014997629 crossrefType "journal-article" @default.
• W2014997629 hasAuthorship W2014997629A5003977888 @default.
• W2014997629 hasAuthorship W2014997629A5008860230 @default.
• W2014997629 hasAuthorship W2014997629A5022116081 @default.
• W2014997629 hasAuthorship W2014997629A5027405014 @default.
• W2014997629 hasAuthorship W2014997629A5034267164 @default.
• W2014997629 hasAuthorship W2014997629A5043884920 @default.
• W2014997629 hasConcept C120806208 @default.
• W2014997629 hasConcept C127313418 @default.
• W2014997629 hasConcept C141646446 @default.
• W2014997629 hasConcept C147717901 @default.
• W2014997629 hasConcept C149347711 @default.
• W2014997629 hasConcept C150999391 @default.
• W2014997629 hasConcept C151730666 @default.
• W2014997629 hasConcept C167284885 @default.
• W2014997629 hasConcept C17409809 @default.
• W2014997629 hasConcept C180492444 @default.
• W2014997629 hasConcept C192241223 @default.
• W2014997629 hasConcept C193429443 @default.
• W2014997629 hasConcept C202746551 @default.
• W2014997629 hasConcept C2776698055 @default.
• W2014997629 hasConcept C2778849375 @default.
• W2014997629 hasConcept C2779430719 @default.
• W2014997629 hasConcept C58097730 @default.
• W2014997629 hasConcept C5900021 @default.
• W2014997629 hasConcept C63379926 @default.
• W2014997629 hasConcept C77928131 @default.
• W2014997629 hasConcept C93253190 @default.
• W2014997629 hasConcept C95628711 @default.
• W2014997629 hasConceptScore W2014997629C120806208 @default.
• W2014997629 hasConceptScore W2014997629C127313418 @default.
• W2014997629 hasConceptScore W2014997629C141646446 @default.
• W2014997629 hasConceptScore W2014997629C147717901 @default.
• W2014997629 hasConceptScore W2014997629C149347711 @default.
• W2014997629 hasConceptScore W2014997629C150999391 @default.
• W2014997629 hasConceptScore W2014997629C151730666 @default.
• W2014997629 hasConceptScore W2014997629C167284885 @default.
• W2014997629 hasConceptScore W2014997629C17409809 @default.
• W2014997629 hasConceptScore W2014997629C180492444 @default.
• W2014997629 hasConceptScore W2014997629C192241223 @default.
• W2014997629 hasConceptScore W2014997629C193429443 @default.
• W2014997629 hasConceptScore W2014997629C202746551 @default.
• W2014997629 hasConceptScore W2014997629C2776698055 @default.
• W2014997629 hasConceptScore W2014997629C2778849375 @default.
• W2014997629 hasConceptScore W2014997629C2779430719 @default.
• W2014997629 hasConceptScore W2014997629C58097730 @default.
• W2014997629 hasConceptScore W2014997629C5900021 @default.
• W2014997629 hasConceptScore W2014997629C63379926 @default.

• next