FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1993392703> ?p ?o ?g. }

• W1993392703 endingPage "53" @default.
• W1993392703 startingPage "39" @default.
• W1993392703 abstract "Alkaline magmatism during the late Proterozoic is an important event in the northern part of the South Indian granulite terrain. A number of alkaline plutons comprising saturated syenite and ultramafic rocks often associated with carbonatite are found localized along NEHYPHEN;SW trending lineaments, which are considered as deep crustal fractures. Along one such lineament, the alkaline complexes of Yelagiri, Sevattur and Samalpatti have intruded into the country rocks comprising epidote hornblende gneiss. The isotope characteristics and geochemistry of Yelagiri and Sevattur plutons are examined in this paper. Whole rock Rbhyphen;Sr isochron ages of the Yelagiri and Sevattur syenites are 757±32 Ma and 756±11 Ma respectively. The close spatial relationship, similarities in age, mineralogical and geochemical characteristics of these plutons strongly suggest their close genetic relationship. The initial Sr and Nd isotope ratios of the Sevattur carbonatites suggest their derivation from an alkali metal and LREE enriched mantle source. However, the silicate rocks of the Yelagiri and Sevattur plutons have distinctly different isotopic characteristics from this enriched mantle source. Combined geochemical and isotopic characteristics of these silicate rocks indicate that silicate rocks of both plutons are derived independently from isotopically different sources from those of carbonatites. Moreover, comparison with the isotopic characteristics of Archean crustal rocks in South India indicates that the source regions of both silicate rocks are lowerhyphen;crustal portions, which are deeper than any other crustal portion exposed in South India, or isotopically metasomatized crustal portions by volatile influx from carbonatite." @default.
• W1993392703 created "2016-06-24" @default.
• W1993392703 creator A5081358924 @default.
• W1993392703 date "2000-01-01" @default.
• W1993392703 modified "2023-10-16" @default.
• W1993392703 title "Rb-Sr Geochronology, Nd-Sr Isotopes and Whole Rock Geochemistry of Yelagiri and Sevattur Syenites, Tamil Nadu, South India" @default.
• W1993392703 cites W1508298471 @default.
• W1993392703 cites W1526466609 @default.
• W1993392703 cites W1964058583 @default.
• W1993392703 cites W1966409112 @default.
• W1993392703 cites W1968037380 @default.
• W1993392703 cites W1970595751 @default.
• W1993392703 cites W1971513400 @default.
• W1993392703 cites W1971844979 @default.
• W1993392703 cites W1971892298 @default.
• W1993392703 cites W1991788391 @default.
• W1993392703 cites W1993810962 @default.
• W1993392703 cites W2008281306 @default.
• W1993392703 cites W2012519141 @default.
• W1993392703 cites W2032091086 @default.
• W1993392703 cites W2046710075 @default.
• W1993392703 cites W2052055789 @default.
• W1993392703 cites W2055950106 @default.
• W1993392703 cites W2076719789 @default.
• W1993392703 cites W2083378408 @default.
• W1993392703 cites W2090278244 @default.
• W1993392703 cites W2146267965 @default.
• W1993392703 cites W2156737155 @default.
• W1993392703 cites W2157271226 @default.
• W1993392703 cites W2161180418 @default.
• W1993392703 cites W2410858044 @default.
• W1993392703 cites W2520407013 @default.
• W1993392703 cites W2561404590 @default.
• W1993392703 cites W2581637824 @default.
• W1993392703 cites W2598779080 @default.
• W1993392703 cites W2599668627 @default.
• W1993392703 cites W425929355 @default.
• W1993392703 cites W46372954 @default.
• W1993392703 cites W581790785 @default.
• W1993392703 cites W2276768444 @default.
• W1993392703 cites W2304842675 @default.
• W1993392703 cites W2587408784 @default.
• W1993392703 cites W2603464972 @default.
• W1993392703 doi "https://doi.org/10.1016/s1342-937x(05)70056-3" @default.
• W1993392703 hasPublicationYear "2000" @default.
• W1993392703 type Work @default.
• W1993392703 sameAs 1993392703 @default.
• W1993392703 citedByCount "58" @default.
• W1993392703 countsByYear W19933927032012 @default.
• W1993392703 countsByYear W19933927032013 @default.
• W1993392703 countsByYear W19933927032014 @default.
• W1993392703 countsByYear W19933927032015 @default.
• W1993392703 countsByYear W19933927032016 @default.
• W1993392703 countsByYear W19933927032017 @default.
• W1993392703 countsByYear W19933927032018 @default.
• W1993392703 countsByYear W19933927032019 @default.
• W1993392703 countsByYear W19933927032020 @default.
• W1993392703 countsByYear W19933927032021 @default.
• W1993392703 countsByYear W19933927032022 @default.
• W1993392703 countsByYear W19933927032023 @default.
• W1993392703 crossrefType "journal-article" @default.
• W1993392703 hasAuthorship W1993392703A5081358924 @default.
• W1993392703 hasConcept C127313418 @default.
• W1993392703 hasConcept C140441402 @default.
• W1993392703 hasConcept C149347711 @default.
• W1993392703 hasConcept C151730666 @default.
• W1993392703 hasConcept C171701179 @default.
• W1993392703 hasConcept C17409809 @default.
• W1993392703 hasConcept C195081551 @default.
• W1993392703 hasConcept C202746551 @default.
• W1993392703 hasConcept C26687426 @default.
• W1993392703 hasConcept C2777212541 @default.
• W1993392703 hasConcept C2777229588 @default.
• W1993392703 hasConcept C2778849375 @default.
• W1993392703 hasConcept C2779870107 @default.
• W1993392703 hasConcept C34122518 @default.
• W1993392703 hasConcept C487381 @default.
• W1993392703 hasConcept C5900021 @default.
• W1993392703 hasConcept C67236022 @default.
• W1993392703 hasConcept C77928131 @default.
• W1993392703 hasConceptScore W1993392703C127313418 @default.
• W1993392703 hasConceptScore W1993392703C140441402 @default.
• W1993392703 hasConceptScore W1993392703C149347711 @default.
• W1993392703 hasConceptScore W1993392703C151730666 @default.
• W1993392703 hasConceptScore W1993392703C171701179 @default.
• W1993392703 hasConceptScore W1993392703C17409809 @default.
• W1993392703 hasConceptScore W1993392703C195081551 @default.
• W1993392703 hasConceptScore W1993392703C202746551 @default.
• W1993392703 hasConceptScore W1993392703C26687426 @default.
• W1993392703 hasConceptScore W1993392703C2777212541 @default.
• W1993392703 hasConceptScore W1993392703C2777229588 @default.
• W1993392703 hasConceptScore W1993392703C2778849375 @default.
• W1993392703 hasConceptScore W1993392703C2779870107 @default.
• W1993392703 hasConceptScore W1993392703C34122518 @default.
• W1993392703 hasConceptScore W1993392703C487381 @default.
• W1993392703 hasConceptScore W1993392703C5900021 @default.
• W1993392703 hasConceptScore W1993392703C67236022 @default.
• W1993392703 hasConceptScore W1993392703C77928131 @default.

• next