Matches in SemOpenAlex for { <https://semopenalex.org/work/W2037845312> ?p ?o ?g. }
Showing items 1 to 92 of
92
with 100 items per page.
- W2037845312 endingPage "120" @default.
- W2037845312 startingPage "111" @default.
- W2037845312 abstract "Eleven samples of Skye granites, two samples of Torridonian sandstone and one sample of Lewisian gneiss have been analysed for ten rare earth elements (REE) by neutron activation analysis. The granites are representative of the main granite centres and compositional types. All granites have sub-parallel light-REE-enriched patterns with chondrite-normalised Ce(CeN) = 78–263,YbN = 16–60and CeN/YbN = 2.9–8.0. REE patterns for the Lewisian gneiss and Torridonian sandstone are similar to each other, withCeN = 32–61,YbN = 3–5and CeN/YbN = 8–18. These two rock types as well as the Glamaig granite have negligible Eu anomalies (Eu/Eu* > 0.9), and the other granites have Eu/Eu* in the range 0.83-0.34. The REE evidence suggests that Lewisian gneiss or Torridonian sandstone arenot suitable materials from which the granites could be derived by partial melting. The Western Red Hills granite intrusions show a systematic relation of REE content with Eu/Eu*. We suggest that the Glamaig granite is the most primitive, and was derived from a source with no Eu anomaly by fractional crystallization of a more basic magma. The later Western Red Hills granites might then have resulted from further fractional crystallization of magma with a composition like that of the Glamaig granite. The Coire Uaigneich and Eastern Red Hills granites may also be products of fractional crystallization, but from different magmas to those parental to the Western Red Hills granites. The basaltic parent magmas of the Skye granites may be “continental” tholeiites derived by interaction of basalt magma with Lewisian gneiss." @default.
- W2037845312 created "2016-06-24" @default.
- W2037845312 creator A5006355932 @default.
- W2037845312 creator A5036871405 @default.
- W2037845312 creator A5088703885 @default.
- W2037845312 date "1977-08-01" @default.
- W2037845312 modified "2023-10-18" @default.
- W2037845312 title "Rare earth evidence concerning the origin of granites of the Isle of Skye, northwest Scotland" @default.
- W2037845312 cites W1964149694 @default.
- W2037845312 cites W1970046654 @default.
- W2037845312 cites W1979120126 @default.
- W2037845312 cites W1983145904 @default.
- W2037845312 cites W1998358801 @default.
- W2037845312 cites W2000052978 @default.
- W2037845312 cites W2018255021 @default.
- W2037845312 cites W2027862110 @default.
- W2037845312 cites W2037106619 @default.
- W2037845312 cites W2037989335 @default.
- W2037845312 cites W2039303705 @default.
- W2037845312 cites W2039989027 @default.
- W2037845312 cites W2044990638 @default.
- W2037845312 cites W2047218915 @default.
- W2037845312 cites W2054334712 @default.
- W2037845312 cites W2054578927 @default.
- W2037845312 cites W2058312784 @default.
- W2037845312 cites W2059429492 @default.
- W2037845312 cites W2060289092 @default.
- W2037845312 cites W2066893568 @default.
- W2037845312 cites W2082031187 @default.
- W2037845312 cites W2088341793 @default.
- W2037845312 cites W2088823453 @default.
- W2037845312 cites W2094469879 @default.
- W2037845312 cites W2132860549 @default.
- W2037845312 cites W2143836610 @default.
- W2037845312 cites W2151802570 @default.
- W2037845312 cites W2159678495 @default.
- W2037845312 cites W2313877506 @default.
- W2037845312 cites W2315316925 @default.
- W2037845312 cites W2326950840 @default.
- W2037845312 cites W2327308766 @default.
- W2037845312 cites W2328994655 @default.
- W2037845312 doi "https://doi.org/10.1016/0012-821x(77)90192-3" @default.
- W2037845312 hasPublicationYear "1977" @default.
- W2037845312 type Work @default.
- W2037845312 sameAs 2037845312 @default.
- W2037845312 citedByCount "29" @default.
- W2037845312 countsByYear W20378453122013 @default.
- W2037845312 crossrefType "journal-article" @default.
- W2037845312 hasAuthorship W2037845312A5006355932 @default.
- W2037845312 hasAuthorship W2037845312A5036871405 @default.
- W2037845312 hasAuthorship W2037845312A5088703885 @default.
- W2037845312 hasConcept C11872896 @default.
- W2037845312 hasConcept C120806208 @default.
- W2037845312 hasConcept C127313418 @default.
- W2037845312 hasConcept C161509811 @default.
- W2037845312 hasConcept C171701179 @default.
- W2037845312 hasConcept C17409809 @default.
- W2037845312 hasConcept C183222429 @default.
- W2037845312 hasConcept C26687426 @default.
- W2037845312 hasConcept C2778849375 @default.
- W2037845312 hasConcept C79572550 @default.
- W2037845312 hasConceptScore W2037845312C11872896 @default.
- W2037845312 hasConceptScore W2037845312C120806208 @default.
- W2037845312 hasConceptScore W2037845312C127313418 @default.
- W2037845312 hasConceptScore W2037845312C161509811 @default.
- W2037845312 hasConceptScore W2037845312C171701179 @default.
- W2037845312 hasConceptScore W2037845312C17409809 @default.
- W2037845312 hasConceptScore W2037845312C183222429 @default.
- W2037845312 hasConceptScore W2037845312C26687426 @default.
- W2037845312 hasConceptScore W2037845312C2778849375 @default.
- W2037845312 hasConceptScore W2037845312C79572550 @default.
- W2037845312 hasIssue "1" @default.
- W2037845312 hasLocation W20378453121 @default.
- W2037845312 hasOpenAccess W2037845312 @default.
- W2037845312 hasPrimaryLocation W20378453121 @default.
- W2037845312 hasRelatedWork W1588988523 @default.
- W2037845312 hasRelatedWork W2018717732 @default.
- W2037845312 hasRelatedWork W2029957077 @default.
- W2037845312 hasRelatedWork W2495537788 @default.
- W2037845312 hasRelatedWork W2781892514 @default.
- W2037845312 hasRelatedWork W2902593388 @default.
- W2037845312 hasRelatedWork W3018450081 @default.
- W2037845312 hasRelatedWork W3185765820 @default.
- W2037845312 hasRelatedWork W3192996540 @default.
- W2037845312 hasRelatedWork W3214232781 @default.
- W2037845312 hasVolume "36" @default.
- W2037845312 isParatext "false" @default.
- W2037845312 isRetracted "false" @default.
- W2037845312 magId "2037845312" @default.
- W2037845312 workType "article" @default.