FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020006343> ?p ?o ?g. }

• W2020006343 endingPage "588" @default.
• W2020006343 startingPage "553" @default.
• W2020006343 abstract "Synopsis This study of the mineralogy and metamorphism of the Moine schists approaches the problem through consideration of the chemical composition of the minerals. The principal minerals of the Moine schists are studied individually, thirty-three new analyses of minerals being given, with four of schists. For all but six analyses the trace elements have been determined and are tabulated. Muscovites, biotites and garnets all show variation of composition with increasing metamorphic grade, respectively with decreasing Fe 2 O 3 and SiO 2 , increasing MgO and Al 2 O 3 , and decreasing CaO plus increasing MgO, these being only the principal variations. The crystal chemistry of the muscovites, biotites and garnets is briefly discussed. Some new data are presented for the relationship of plagioclase and epidote, a relationship which can only be used with extreme caution to indicate metamorphic grade. A dependence of the incidence of a sutured quartz aggregate in psammitic schists upon the microcline content is noted, and it is suggested that the incidence of the breakdown of quartz under the combined effect of temperature (the dominant cause), stress and potassio solutions, all active in the core, is responsible for the production of the core-envelope boundary. This boundary transgresses the strike; within it retrogressive changes have converted Garnet-zone schists to Biotite-zone schists, but outside it the only retrogressive change is garnet to chlorite. The retrogressive metamorphism formed a distinct episode separated from the initial regional metamorphism by an unknown time-interval; during the second metamorphism isotherms were concentric with the dome, declining outwards. The evidence of an epidiorite from the west coast of Morar suggests that during the first metamorphism the zonal state there was that of the Dalradian Biotite-zone; “almandine” garnets in the adjacent schists are extremely rich in CaO and are in equilibrium with microcline." @default.
• W2020006343 created "2016-06-24" @default.
• W2020006343 creator A5086319178 @default.
• W2020006343 date "1959-01-01" @default.
• W2020006343 modified "2023-10-11" @default.
• W2020006343 title "XXV.—The Mineralogy and Metamorphism of the Moine Schists of the Morar and Knoydart Districts of Inverness-shire" @default.
• W2020006343 cites W1965554698 @default.
• W2020006343 cites W1967878753 @default.
• W2020006343 cites W1973060577 @default.
• W2020006343 cites W1973508315 @default.
• W2020006343 cites W1974909072 @default.
• W2020006343 cites W1994077914 @default.
• W2020006343 cites W1995374434 @default.
• W2020006343 cites W1998233770 @default.
• W2020006343 cites W2004976151 @default.
• W2020006343 cites W2062584669 @default.
• W2020006343 cites W2071510907 @default.
• W2020006343 cites W2086712362 @default.
• W2020006343 cites W2098300656 @default.
• W2020006343 cites W2101481447 @default.
• W2020006343 cites W2108505672 @default.
• W2020006343 cites W2118225311 @default.
• W2020006343 cites W2130103298 @default.
• W2020006343 cites W2170270570 @default.
• W2020006343 cites W2320415031 @default.
• W2020006343 cites W2322565344 @default.
• W2020006343 cites W2324049844 @default.
• W2020006343 cites W2324485733 @default.
• W2020006343 cites W2325236507 @default.
• W2020006343 cites W2328013432 @default.
• W2020006343 cites W2331614215 @default.
• W2020006343 cites W2478496673 @default.
• W2020006343 cites W4253560639 @default.
• W2020006343 doi "https://doi.org/10.1017/s0080456800003148" @default.
• W2020006343 hasPublicationYear "1959" @default.
• W2020006343 type Work @default.
• W2020006343 sameAs 2020006343 @default.
• W2020006343 citedByCount "93" @default.
• W2020006343 countsByYear W20200063432012 @default.
• W2020006343 countsByYear W20200063432021 @default.
• W2020006343 crossrefType "journal-article" @default.
• W2020006343 hasAuthorship W2020006343A5086319178 @default.
• W2020006343 hasConcept C101139013 @default.
• W2020006343 hasConcept C112764850 @default.
• W2020006343 hasConcept C127313418 @default.
• W2020006343 hasConcept C151730666 @default.
• W2020006343 hasConcept C17409809 @default.
• W2020006343 hasConcept C199289684 @default.
• W2020006343 hasConcept C26687426 @default.
• W2020006343 hasConcept C2777229588 @default.
• W2020006343 hasConcept C2777844515 @default.
• W2020006343 hasConcept C2779870107 @default.
• W2020006343 hasConceptScore W2020006343C101139013 @default.
• W2020006343 hasConceptScore W2020006343C112764850 @default.
• W2020006343 hasConceptScore W2020006343C127313418 @default.
• W2020006343 hasConceptScore W2020006343C151730666 @default.
• W2020006343 hasConceptScore W2020006343C17409809 @default.
• W2020006343 hasConceptScore W2020006343C199289684 @default.
• W2020006343 hasConceptScore W2020006343C26687426 @default.
• W2020006343 hasConceptScore W2020006343C2777229588 @default.
• W2020006343 hasConceptScore W2020006343C2777844515 @default.
• W2020006343 hasConceptScore W2020006343C2779870107 @default.
• W2020006343 hasIssue "3" @default.
• W2020006343 hasLocation W20200063431 @default.
• W2020006343 hasOpenAccess W2020006343 @default.
• W2020006343 hasPrimaryLocation W20200063431 @default.
• W2020006343 hasRelatedWork W1006855143 @default.
• W2020006343 hasRelatedWork W1985755952 @default.
• W2020006343 hasRelatedWork W1994586314 @default.
• W2020006343 hasRelatedWork W1998233770 @default.
• W2020006343 hasRelatedWork W2375963570 @default.
• W2020006343 hasRelatedWork W2383722626 @default.
• W2020006343 hasRelatedWork W2398431780 @default.
• W2020006343 hasRelatedWork W2399624486 @default.
• W2020006343 hasRelatedWork W4239299955 @default.
• W2020006343 hasRelatedWork W635132688 @default.
• W2020006343 hasVolume "63" @default.
• W2020006343 isParatext "false" @default.
• W2020006343 isRetracted "false" @default.
• W2020006343 magId "2020006343" @default.
• W2020006343 workType "article" @default.