FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2004169477> ?p ?o ?g. }

• W2004169477 endingPage "728" @default.
• W2004169477 startingPage "713" @default.
• W2004169477 abstract "Quartz-monzodiorite is generally considered to represent the parent magma of high-Mg quartz-monzodiorite plutonic suites; thus such suites are thought to be melts from a metasomatized mantle wedge. It is proposed here that hornblende tonalite, which is present in the feeder dikes of high-Mg quartz-monzodiorite plutonic suites, better represents the parental magma. Hornblende tonalite has a higher compatible element content with a relatively lower incompatible element content and a lower ratio than quartz-monzodiorite, suggesting that the tonalite is the more primitive magma of the suite. The hornblendite unit of the high-Mg quartz-monzodiorite plutonic suite is interpreted to represent the cumulate, and the quartz-monzodiorite the differentiated liquid. To test this hypothesis and explain the differentiation of the units of a high-Mg quartz-monzodiorite plutonic suite, the Houghton pluton in the northern Abitibi greenstone belt, Quebec, was studied. Results show that crystal fractionation and equilibrium crystallization cannot sufficiently enrich incompatible elements in the quartz-monzodiorite while keeping the compatible element contents high. Feeder dike petrography suggests that the magma chamber was periodically replenished. The model that best explains the formation of the different units of this suite is a periodically replenished magma chamber with a crystallization sequence of hornblende followed by hornblende and plagioclase. Such a magma chamber undergoing crystal fractionation will produce the high incompatible and compatible element contents typical of quartz-monzodiorite magmas. Not all quartz-monzodiorite magmas of the site can be explained by a replenishment of the hornblende tonalite. As identified in the feeder system, the replenishing magma changed at some time to one represented by leucotonalite-to-quartz-diorite. By changing the replenishing magma from the hornblende tonalite to the leucotonalite-to-quartz-diorite unit, after the differentiated liquid reached 64% , it is possible to model all the units in the plutonic suite. The hornblendite unit can be easily modeled for the major oxides, but the inclusion or exclusion of accessory phases rich in trace elements (allanite) in the samples renders trace element behavior erratic, and the hornblendite cannot be successfully modeled." @default.
• W2004169477 created "2016-06-24" @default.
• W2004169477 creator A5006897360 @default.
• W2004169477 date "1996-11-01" @default.
• W2004169477 modified "2023-10-06" @default.
• W2004169477 title "Archean High-Mg Quartz-Monzodiorite Suite: A Re-Evaluation of the Parental Magma and Differentiation" @default.
• W2004169477 cites W1640775606 @default.
• W2004169477 cites W1675648967 @default.
• W2004169477 cites W1967156352 @default.
• W2004169477 cites W1976233827 @default.
• W2004169477 cites W1979350315 @default.
• W2004169477 cites W1983139271 @default.
• W2004169477 cites W1984463945 @default.
• W2004169477 cites W2006834372 @default.
• W2004169477 cites W2009615347 @default.
• W2004169477 cites W2013068692 @default.
• W2004169477 cites W2016282152 @default.
• W2004169477 cites W2022463607 @default.
• W2004169477 cites W2024575502 @default.
• W2004169477 cites W2027186281 @default.
• W2004169477 cites W2028197785 @default.
• W2004169477 cites W2032877876 @default.
• W2004169477 cites W2035097203 @default.
• W2004169477 cites W2040049557 @default.
• W2004169477 cites W2040221117 @default.
• W2004169477 cites W2041205225 @default.
• W2004169477 cites W2045684026 @default.
• W2004169477 cites W2046961523 @default.
• W2004169477 cites W2048344865 @default.
• W2004169477 cites W2057652698 @default.
• W2004169477 cites W2058889826 @default.
• W2004169477 cites W2060878189 @default.
• W2004169477 cites W2061523635 @default.
• W2004169477 cites W2062218969 @default.
• W2004169477 cites W2067924308 @default.
• W2004169477 cites W2072699489 @default.
• W2004169477 cites W2080494759 @default.
• W2004169477 cites W2081839864 @default.
• W2004169477 cites W2083367334 @default.
• W2004169477 cites W2096389188 @default.
• W2004169477 cites W2104589541 @default.
• W2004169477 cites W2116704356 @default.
• W2004169477 cites W2157181776 @default.
• W2004169477 cites W2312559920 @default.
• W2004169477 cites W2332879341 @default.
• W2004169477 cites W2405643826 @default.
• W2004169477 cites W2980936855 @default.
• W2004169477 doi "https://doi.org/10.1086/629864" @default.
• W2004169477 hasPublicationYear "1996" @default.
• W2004169477 type Work @default.
• W2004169477 sameAs 2004169477 @default.
• W2004169477 citedByCount "10" @default.
• W2004169477 countsByYear W20041694772012 @default.
• W2004169477 countsByYear W20041694772014 @default.
• W2004169477 countsByYear W20041694772015 @default.
• W2004169477 countsByYear W20041694772018 @default.
• W2004169477 countsByYear W20041694772019 @default.
• W2004169477 countsByYear W20041694772020 @default.
• W2004169477 countsByYear W20041694772021 @default.
• W2004169477 crossrefType "journal-article" @default.
• W2004169477 hasAuthorship W2004169477A5006897360 @default.
• W2004169477 hasConcept C11872896 @default.
• W2004169477 hasConcept C120806208 @default.
• W2004169477 hasConcept C127313418 @default.
• W2004169477 hasConcept C149347711 @default.
• W2004169477 hasConcept C151730666 @default.
• W2004169477 hasConcept C161509811 @default.
• W2004169477 hasConcept C167236342 @default.
• W2004169477 hasConcept C167284885 @default.
• W2004169477 hasConcept C17409809 @default.
• W2004169477 hasConcept C183222429 @default.
• W2004169477 hasConcept C2777212541 @default.
• W2004169477 hasConcept C2777229588 @default.
• W2004169477 hasConcept C2779181077 @default.
• W2004169477 hasConcept C2779870107 @default.
• W2004169477 hasConcept C34122518 @default.
• W2004169477 hasConcept C5900021 @default.
• W2004169477 hasConcept C77928131 @default.
• W2004169477 hasConcept C9566828 @default.
• W2004169477 hasConceptScore W2004169477C11872896 @default.
• W2004169477 hasConceptScore W2004169477C120806208 @default.
• W2004169477 hasConceptScore W2004169477C127313418 @default.
• W2004169477 hasConceptScore W2004169477C149347711 @default.
• W2004169477 hasConceptScore W2004169477C151730666 @default.
• W2004169477 hasConceptScore W2004169477C161509811 @default.
• W2004169477 hasConceptScore W2004169477C167236342 @default.
• W2004169477 hasConceptScore W2004169477C167284885 @default.
• W2004169477 hasConceptScore W2004169477C17409809 @default.
• W2004169477 hasConceptScore W2004169477C183222429 @default.
• W2004169477 hasConceptScore W2004169477C2777212541 @default.
• W2004169477 hasConceptScore W2004169477C2777229588 @default.
• W2004169477 hasConceptScore W2004169477C2779181077 @default.
• W2004169477 hasConceptScore W2004169477C2779870107 @default.
• W2004169477 hasConceptScore W2004169477C34122518 @default.
• W2004169477 hasConceptScore W2004169477C5900021 @default.
• W2004169477 hasConceptScore W2004169477C77928131 @default.
• W2004169477 hasConceptScore W2004169477C9566828 @default.
• W2004169477 hasIssue "6" @default.

• next