FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2030397687> ?p ?o ?g. }

• W2030397687 endingPage "101" @default.
• W2030397687 startingPage "95" @default.
• W2030397687 abstract "The La/Nb ratio (<1.4) and the Ni concentration (>30 ppm at a Mg number of 40) in oceanic plateau basalts and MORB provide a useful index to distinguish them from arc basalts. MORB can generally be distinguished from plateau basalts by their lower Nb contents (<3 ppm) and lower Nb/Y ratios (<0.1). The La/Nb ratio and Ni contents of mafic lower crustal xenoliths indicate that at most xenolith sites, both arc and plume-related components occur in the lower crust. Considered as a whole, mafic xenolith data suggest that about one third of the post-Archean lower continental crust is composed of mafic rocks from mantle plume sources (accreted oceanic plateaus or mafic underplate), and the remainder come chiefly from arc sources. Because both crustal and host magma contamination should raise La/Nb ratios in xenoliths, the value of one third is a minimum for the plume component in the lower crust." @default.
• W2030397687 created "2016-06-24" @default.
• W2030397687 creator A5013541003 @default.
• W2030397687 date "1999-01-01" @default.
• W2030397687 modified "2023-10-11" @default.
• W2030397687 title "Mafic crustal xenoliths and the origin of the lower continental crust" @default.
• W2030397687 cites W1145830493 @default.
• W2030397687 cites W1509769237 @default.
• W2030397687 cites W1892858296 @default.
• W2030397687 cites W1965258029 @default.
• W2030397687 cites W1972781742 @default.
• W2030397687 cites W1975042776 @default.
• W2030397687 cites W1975754127 @default.
• W2030397687 cites W1980482433 @default.
• W2030397687 cites W1982286853 @default.
• W2030397687 cites W1990832360 @default.
• W2030397687 cites W1994059533 @default.
• W2030397687 cites W1998842874 @default.
• W2030397687 cites W2003493304 @default.
• W2030397687 cites W2005778537 @default.
• W2030397687 cites W2008266762 @default.
• W2030397687 cites W2020168402 @default.
• W2030397687 cites W2031605536 @default.
• W2030397687 cites W2038213764 @default.
• W2030397687 cites W2041176411 @default.
• W2030397687 cites W2043789670 @default.
• W2030397687 cites W2048960899 @default.
• W2030397687 cites W2050438014 @default.
• W2030397687 cites W2060407598 @default.
• W2030397687 cites W2062846503 @default.
• W2030397687 cites W2063511986 @default.
• W2030397687 cites W2064121765 @default.
• W2030397687 cites W2064496902 @default.
• W2030397687 cites W2070870472 @default.
• W2030397687 cites W2080852722 @default.
• W2030397687 cites W2081403281 @default.
• W2030397687 cites W2091835213 @default.
• W2030397687 cites W2093983309 @default.
• W2030397687 cites W2109518222 @default.
• W2030397687 cites W2115274569 @default.
• W2030397687 cites W2125726360 @default.
• W2030397687 cites W2151841546 @default.
• W2030397687 cites W2157267921 @default.
• W2030397687 cites W2314378019 @default.
• W2030397687 cites W2329034801 @default.
• W2030397687 cites W4237577704 @default.
• W2030397687 cites W53138660 @default.
• W2030397687 doi "https://doi.org/10.1016/s0024-4937(98)00056-5" @default.
• W2030397687 hasPublicationYear "1999" @default.
• W2030397687 type Work @default.
• W2030397687 sameAs 2030397687 @default.
• W2030397687 citedByCount "114" @default.
• W2030397687 countsByYear W20303976872012 @default.
• W2030397687 countsByYear W20303976872013 @default.
• W2030397687 countsByYear W20303976872014 @default.
• W2030397687 countsByYear W20303976872015 @default.
• W2030397687 countsByYear W20303976872016 @default.
• W2030397687 countsByYear W20303976872017 @default.
• W2030397687 countsByYear W20303976872018 @default.
• W2030397687 countsByYear W20303976872019 @default.
• W2030397687 countsByYear W20303976872020 @default.
• W2030397687 countsByYear W20303976872021 @default.
• W2030397687 countsByYear W20303976872022 @default.
• W2030397687 countsByYear W20303976872023 @default.
• W2030397687 crossrefType "journal-article" @default.
• W2030397687 hasAuthorship W2030397687A5013541003 @default.
• W2030397687 hasConcept C127313418 @default.
• W2030397687 hasConcept C141646446 @default.
• W2030397687 hasConcept C147894010 @default.
• W2030397687 hasConcept C151730666 @default.
• W2030397687 hasConcept C154200439 @default.
• W2030397687 hasConcept C161509811 @default.
• W2030397687 hasConcept C167284885 @default.
• W2030397687 hasConcept C16942324 @default.
• W2030397687 hasConcept C17409809 @default.
• W2030397687 hasConcept C2776698055 @default.
• W2030397687 hasConcept C42796848 @default.
• W2030397687 hasConcept C58097730 @default.
• W2030397687 hasConcept C5900021 @default.
• W2030397687 hasConcept C77928131 @default.
• W2030397687 hasConceptScore W2030397687C127313418 @default.
• W2030397687 hasConceptScore W2030397687C141646446 @default.
• W2030397687 hasConceptScore W2030397687C147894010 @default.
• W2030397687 hasConceptScore W2030397687C151730666 @default.
• W2030397687 hasConceptScore W2030397687C154200439 @default.
• W2030397687 hasConceptScore W2030397687C161509811 @default.
• W2030397687 hasConceptScore W2030397687C167284885 @default.
• W2030397687 hasConceptScore W2030397687C16942324 @default.
• W2030397687 hasConceptScore W2030397687C17409809 @default.
• W2030397687 hasConceptScore W2030397687C2776698055 @default.
• W2030397687 hasConceptScore W2030397687C42796848 @default.
• W2030397687 hasConceptScore W2030397687C58097730 @default.
• W2030397687 hasConceptScore W2030397687C5900021 @default.
• W2030397687 hasConceptScore W2030397687C77928131 @default.
• W2030397687 hasIssue "1" @default.
• W2030397687 hasLocation W20303976871 @default.
• W2030397687 hasOpenAccess W2030397687 @default.
• W2030397687 hasPrimaryLocation W20303976871 @default.

• next