FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013828117> ?p ?o ?g. }

• W2013828117 endingPage "124" @default.
• W2013828117 startingPage "105" @default.
• W2013828117 abstract "Synopsis Closed-basin deposits of the Stoer Group and Diabaig Formation were locally derived from Lewisian felsic and mafic rocks in semi-arid to temperate climates. For open-basin deposits of the Applecross and Aultbea Formations, provenance was Grenville-age rocks and older Pro-terozoic and Archaean rocks in Laurentia, west of the rift basin. Petrography shows that detrital Ca-plagioclase, K-feldspar, and matrix clays were albitized during diagenesis. Evaluation of geochemical data for Stoer and Torridonian Group sedimentary rocks indicates widespread sodium metasomatism in these rocks. For the very sodic Stoer Group sandstones and siltstones, containing as much as 6% Na 2 O, up to 2–3% Na 2 O was added, during diagenesis, to the detrital sediments. Similar Na-metasomatism occurred in the Diabaig and Cailleach Head sandstones. The meta-somatic process involved evaporative concentration of salts in closed basin groundwaters yielding Na-rich brines which reacted with detrital silicates to develop authigenic albite. Calcium, released from detrital plagioclase during diagenesis, is resident in authigenic epidote or calcite, depending on local p CO 2 . During metasomatism, potassium minerals were replaced by albite and the liberated K was incorporated into illite-mica in shales. Granulite facies provenance is indicated for some of the clastics by K/Rb of 465–1295, much higher than common crustal K/Rb values. In open-basin deposits of the Applecross and Aultbea Formations, low abundances of Fe, Mg, Co, Cr, and Ni indicate little mafic and/or ultramafic rock in the source area. Petrography indicates that these immature sediments include some recycled sedimentary or metasedimentary rocks and were developed in a temperate-humid climate where moderate weathering removed considerable plagioclase from the source rocks prior to transport and deposition." @default.
• W2013828117 created "2016-06-24" @default.
• W2013828117 creator A5016798817 @default.
• W2013828117 creator A5062630474 @default.
• W2013828117 date "1997-11-01" @default.
• W2013828117 modified "2023-09-29" @default.
• W2013828117 title "Mineralogy, geochemistry, provenance and sodium metasomatism of Torridonian rift basin clastic rocks, NW Scotland" @default.
• W2013828117 cites W141271007 @default.
• W2013828117 cites W141993106 @default.
• W2013828117 cites W1942172993 @default.
• W2013828117 cites W1965701586 @default.
• W2013828117 cites W1965969122 @default.
• W2013828117 cites W1978488084 @default.
• W2013828117 cites W1982638607 @default.
• W2013828117 cites W1985764692 @default.
• W2013828117 cites W1986550275 @default.
• W2013828117 cites W1995418569 @default.
• W2013828117 cites W1998664830 @default.
• W2013828117 cites W1998772895 @default.
• W2013828117 cites W2004054556 @default.
• W2013828117 cites W2012894752 @default.
• W2013828117 cites W2016471681 @default.
• W2013828117 cites W2021027768 @default.
• W2013828117 cites W2021300589 @default.
• W2013828117 cites W2024317509 @default.
• W2013828117 cites W2025969837 @default.
• W2013828117 cites W2029282432 @default.
• W2013828117 cites W2032082002 @default.
• W2013828117 cites W2034741082 @default.
• W2013828117 cites W2040385620 @default.
• W2013828117 cites W2050120676 @default.
• W2013828117 cites W2060262671 @default.
• W2013828117 cites W2066293722 @default.
• W2013828117 cites W2079198463 @default.
• W2013828117 cites W2080452127 @default.
• W2013828117 cites W2086913103 @default.
• W2013828117 cites W2091978794 @default.
• W2013828117 cites W2099635912 @default.
• W2013828117 cites W2103077931 @default.
• W2013828117 cites W2106087356 @default.
• W2013828117 cites W2142933079 @default.
• W2013828117 cites W2142935973 @default.
• W2013828117 cites W2148602589 @default.
• W2013828117 cites W2148618920 @default.
• W2013828117 cites W2161503203 @default.
• W2013828117 cites W2165973734 @default.
• W2013828117 cites W2335705700 @default.
• W2013828117 cites W2477262914 @default.
• W2013828117 cites W2481469038 @default.
• W2013828117 cites W25906832 @default.
• W2013828117 cites W4211104829 @default.
• W2013828117 cites W967391294 @default.
• W2013828117 doi "https://doi.org/10.1144/sjg33020105" @default.
• W2013828117 hasPublicationYear "1997" @default.
• W2013828117 type Work @default.
• W2013828117 sameAs 2013828117 @default.
• W2013828117 citedByCount "37" @default.
• W2013828117 countsByYear W20138281172012 @default.
• W2013828117 countsByYear W20138281172014 @default.
• W2013828117 countsByYear W20138281172015 @default.
• W2013828117 countsByYear W20138281172016 @default.
• W2013828117 countsByYear W20138281172017 @default.
• W2013828117 countsByYear W20138281172018 @default.
• W2013828117 countsByYear W20138281172019 @default.
• W2013828117 countsByYear W20138281172020 @default.
• W2013828117 countsByYear W20138281172022 @default.
• W2013828117 countsByYear W20138281172023 @default.
• W2013828117 crossrefType "journal-article" @default.
• W2013828117 hasAuthorship W2013828117A5016798817 @default.
• W2013828117 hasAuthorship W2013828117A5062630474 @default.
• W2013828117 hasConcept C109007969 @default.
• W2013828117 hasConcept C114793014 @default.
• W2013828117 hasConcept C127313418 @default.
• W2013828117 hasConcept C138170599 @default.
• W2013828117 hasConcept C167919410 @default.
• W2013828117 hasConcept C17409809 @default.
• W2013828117 hasConcept C2780049196 @default.
• W2013828117 hasConcept C50682988 @default.
• W2013828117 hasConcept C5900021 @default.
• W2013828117 hasConcept C6494504 @default.
• W2013828117 hasConcept C67236022 @default.
• W2013828117 hasConceptScore W2013828117C109007969 @default.
• W2013828117 hasConceptScore W2013828117C114793014 @default.
• W2013828117 hasConceptScore W2013828117C127313418 @default.
• W2013828117 hasConceptScore W2013828117C138170599 @default.
• W2013828117 hasConceptScore W2013828117C167919410 @default.
• W2013828117 hasConceptScore W2013828117C17409809 @default.
• W2013828117 hasConceptScore W2013828117C2780049196 @default.
• W2013828117 hasConceptScore W2013828117C50682988 @default.
• W2013828117 hasConceptScore W2013828117C5900021 @default.
• W2013828117 hasConceptScore W2013828117C6494504 @default.
• W2013828117 hasConceptScore W2013828117C67236022 @default.
• W2013828117 hasIssue "2" @default.
• W2013828117 hasLocation W20138281171 @default.
• W2013828117 hasOpenAccess W2013828117 @default.
• W2013828117 hasPrimaryLocation W20138281171 @default.
• W2013828117 hasRelatedWork W1967626509 @default.
• W2013828117 hasRelatedWork W2008401539 @default.

• next