FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1994989425> ?p ?o ?g. }

• W1994989425 endingPage "250" @default.
• W1994989425 startingPage "227" @default.
• W1994989425 abstract "Granitoid magmatism spans three Flin Flon Belt evolutionary stages: (i) evolved arc (~1920 Ma) plus early juvenile arc (1904-1880 Ma) plutonism during intraoceanic arc-back-arc formation; (ii) early (1878-1860 Ma) and middle (1860-1844 Ma) successor arc plutonism following accretion and successor arc(s) development and; (iii) late (1843-1826 Ma) successor arc plutonism accompanying successor basin formation and waning arc magmatism. Amphibole-bearing mineralogy, metaluminous compositions, and igneous microgranitoid enclaves indicate derivation from infracrustal sources. Predominance of intermediate calc-alkaline compositions and negative Nb anomalies on normalized patterns over a 46-77 wt.% silica range indicate an arc setting. Basaltic end members indicate important contributions directly from the mantle. ε Nd (T) values are predominately in the range 0 to +4.3, reflecting mixing between depleted mantle melts and an Archean crustal component preserved in evolved arc plutons (-3.9 to -6). Temporal variations include the following: (i) early juvenile arc plutons are low K, high field strength element (HFSE) depleted, with relatively flat rare earth element (REE) patterns and negative Eu anomalies, indicative of low-pressure partial melting - fractionation in the mantle wedge, with residual pyroxene and plagioclase; (ii) early and middle successor arc plutonism is medium K, with steep REE patterns and no Eu anomalies, indicative of input from melting of basaltic sources (likely subducted back-arc oceanic crust) under high-pressure conditions with residual garnet and (or) amphibole and no plagioclase; (iii) late successor arc plutons are high K, more HFSE enriched, with both variable REE pattern slopes and Eu anomalies, indicative of a significant petrogenetic role of recycling of preexisting juvenile arc - accretionary complex crust." @default.
• W1994989425 created "2016-06-24" @default.
• W1994989425 creator A5018560948 @default.
• W1994989425 creator A5043324843 @default.
• W1994989425 creator A5091516703 @default.
• W1994989425 date "1999-02-01" @default.
• W1994989425 modified "2023-10-01" @default.
• W1994989425 title "Geochemical and Nd isotopic evolution of Paleoproterozoic arc-type granitoid magmatism in the Flin Flon Belt, Trans-Hudson orogen, Canada" @default.
• W1994989425 cites W1971685925 @default.
• W1994989425 cites W1979705656 @default.
• W1994989425 cites W1989367202 @default.
• W1994989425 cites W1991430777 @default.
• W1994989425 cites W2000713509 @default.
• W1994989425 cites W2004778581 @default.
• W1994989425 cites W2004780523 @default.
• W1994989425 cites W2006783816 @default.
• W1994989425 cites W2012715340 @default.
• W1994989425 cites W2021987309 @default.
• W1994989425 cites W2022017333 @default.
• W1994989425 cites W2022665116 @default.
• W1994989425 cites W2044630803 @default.
• W1994989425 cites W2049502684 @default.
• W1994989425 cites W2059027044 @default.
• W1994989425 cites W2074054545 @default.
• W1994989425 cites W2077704118 @default.
• W1994989425 cites W2081042784 @default.
• W1994989425 cites W2086755132 @default.
• W1994989425 cites W2105985089 @default.
• W1994989425 cites W2108971421 @default.
• W1994989425 cites W2113009765 @default.
• W1994989425 cites W2126309541 @default.
• W1994989425 cites W2143128079 @default.
• W1994989425 cites W2146396587 @default.
• W1994989425 cites W2148388790 @default.
• W1994989425 cites W2152588796 @default.
• W1994989425 cites W2314224457 @default.
• W1994989425 cites W2316472930 @default.
• W1994989425 cites W2317613525 @default.
• W1994989425 cites W805928198 @default.
• W1994989425 doi "https://doi.org/10.1139/e98-026" @default.
• W1994989425 hasPublicationYear "1999" @default.
• W1994989425 type Work @default.
• W1994989425 sameAs 1994989425 @default.
• W1994989425 citedByCount "45" @default.
• W1994989425 countsByYear W19949894252013 @default.
• W1994989425 countsByYear W19949894252014 @default.
• W1994989425 countsByYear W19949894252016 @default.
• W1994989425 countsByYear W19949894252017 @default.
• W1994989425 countsByYear W19949894252018 @default.
• W1994989425 countsByYear W19949894252019 @default.
• W1994989425 countsByYear W19949894252020 @default.
• W1994989425 countsByYear W19949894252021 @default.
• W1994989425 countsByYear W19949894252022 @default.
• W1994989425 crossrefType "journal-article" @default.
• W1994989425 hasAuthorship W1994989425A5018560948 @default.
• W1994989425 hasAuthorship W1994989425A5043324843 @default.
• W1994989425 hasAuthorship W1994989425A5091516703 @default.
• W1994989425 hasConcept C127313418 @default.
• W1994989425 hasConcept C151730666 @default.
• W1994989425 hasConcept C161509811 @default.
• W1994989425 hasConcept C162973429 @default.
• W1994989425 hasConcept C17409809 @default.
• W1994989425 hasConcept C180870510 @default.
• W1994989425 hasConcept C34122518 @default.
• W1994989425 hasConcept C58097730 @default.
• W1994989425 hasConcept C5900021 @default.
• W1994989425 hasConcept C67236022 @default.
• W1994989425 hasConcept C77928131 @default.
• W1994989425 hasConcept C79572550 @default.
• W1994989425 hasConcept C79605941 @default.
• W1994989425 hasConcept C93253190 @default.
• W1994989425 hasConceptScore W1994989425C127313418 @default.
• W1994989425 hasConceptScore W1994989425C151730666 @default.
• W1994989425 hasConceptScore W1994989425C161509811 @default.
• W1994989425 hasConceptScore W1994989425C162973429 @default.
• W1994989425 hasConceptScore W1994989425C17409809 @default.
• W1994989425 hasConceptScore W1994989425C180870510 @default.
• W1994989425 hasConceptScore W1994989425C34122518 @default.
• W1994989425 hasConceptScore W1994989425C58097730 @default.
• W1994989425 hasConceptScore W1994989425C5900021 @default.
• W1994989425 hasConceptScore W1994989425C67236022 @default.
• W1994989425 hasConceptScore W1994989425C77928131 @default.
• W1994989425 hasConceptScore W1994989425C79572550 @default.
• W1994989425 hasConceptScore W1994989425C79605941 @default.
• W1994989425 hasConceptScore W1994989425C93253190 @default.
• W1994989425 hasIssue "2" @default.
• W1994989425 hasLocation W19949894251 @default.
• W1994989425 hasOpenAccess W1994989425 @default.
• W1994989425 hasPrimaryLocation W19949894251 @default.
• W1994989425 hasRelatedWork W1994989425 @default.
• W1994989425 hasRelatedWork W2039485407 @default.
• W1994989425 hasRelatedWork W2043474890 @default.
• W1994989425 hasRelatedWork W2361053869 @default.
• W1994989425 hasRelatedWork W2478284478 @default.
• W1994989425 hasRelatedWork W2970038550 @default.
• W1994989425 hasRelatedWork W3082763059 @default.
• W1994989425 hasRelatedWork W3120858961 @default.
• W1994989425 hasRelatedWork W3193425371 @default.

• next