Matches in SemOpenAlex for { <https://semopenalex.org/work/W2147003679> ?p ?o ?g. }
- W2147003679 endingPage "298" @default.
- W2147003679 startingPage "281" @default.
- W2147003679 abstract "Abstract Rodingites occur in serpentine‐matrix mélange of the N agasaki metamorphic rocks in J apan. Two types of rodingites can be distinguished on the basis of their mode of occurrence and mineralogical composition. One occurs as dikes, which contain a mineral assemblage of grossular, vesuvianite, diopside, apatite, titanite, and zircon. The other occurs as a block, which consists of zoisite, clinozoisite, diopside, chlorite, apatite, titanite, and zircon. The former type of rodingites posses two types of zircons: prismatic and porous. The prismatic zircons contain primary fluid inclusions indicating their crystallization in the presence of fluids. The porous zircons have extensive fractures filled by zircon, which are indicative of a hydrothermal origin. Both zircon types were thought to have formed under the influence of fluids. U – P b ion probe analyses of prismatic zircons from the rodingites yield a weighted mean age of 108–105 Ma, suggesting the Early Cretaceous as the time of rodingitization in the subduction zone. Hafnium isotopic compositions of prismatic zircons are close to or overlap with the mid ocean ridge basalt ( MORB ) H f isotopic ratio. This indicates that the fluid composition may have been reflected by the MORB composition during rodingitization. On the other hand, the low ε Hf values (11.8–18.9) of porous zircons suggest that they incorporate a small amount of H f from fluid contaminated by subducted sediments. The rodingites are significantly enriched in S r and depleted in large ion lithophile elements ( LILE ) ( C s, R b, B a). The fluid during rodingitization is able to extracts LILEs from the protolith of rodingites and adds S r to the protolith of rodingites. The high field strength elements ( HFSE ) ( Z r, T h, U , N b, T a) concentrations in the rodingites are similar to those of MORB , thus indicate their relatively immobile nature during rodingitization." @default.
- W2147003679 created "2016-06-24" @default.
- W2147003679 creator A5000130543 @default.
- W2147003679 creator A5004999383 @default.
- W2147003679 creator A5010757634 @default.
- W2147003679 creator A5047092458 @default.
- W2147003679 creator A5049038755 @default.
- W2147003679 creator A5054097438 @default.
- W2147003679 creator A5054419460 @default.
- W2147003679 creator A5054716335 @default.
- W2147003679 creator A5071225732 @default.
- W2147003679 date "2014-12-01" @default.
- W2147003679 modified "2023-09-24" @default.
- W2147003679 title "The formation of rodingite in the Nagasaki metamorphic rocks at Nomo Peninsula, Kyushu, Japan - Zircon U-Pb and Hf isotopes and trace element evidence" @default.
- W2147003679 cites W1721380001 @default.
- W2147003679 cites W1871734886 @default.
- W2147003679 cites W1968409933 @default.
- W2147003679 cites W1969812288 @default.
- W2147003679 cites W1969859799 @default.
- W2147003679 cites W1977911355 @default.
- W2147003679 cites W1981207838 @default.
- W2147003679 cites W1986526849 @default.
- W2147003679 cites W1987845890 @default.
- W2147003679 cites W1990479851 @default.
- W2147003679 cites W1990793150 @default.
- W2147003679 cites W2007592351 @default.
- W2147003679 cites W2008045929 @default.
- W2147003679 cites W2008072085 @default.
- W2147003679 cites W2011626356 @default.
- W2147003679 cites W2013658093 @default.
- W2147003679 cites W2018678353 @default.
- W2147003679 cites W2019375822 @default.
- W2147003679 cites W2020819261 @default.
- W2147003679 cites W2025159153 @default.
- W2147003679 cites W2033825567 @default.
- W2147003679 cites W2035145608 @default.
- W2147003679 cites W2039872199 @default.
- W2147003679 cites W2041082912 @default.
- W2147003679 cites W2043269657 @default.
- W2147003679 cites W2051273227 @default.
- W2147003679 cites W2058077530 @default.
- W2147003679 cites W2058646051 @default.
- W2147003679 cites W2060747164 @default.
- W2147003679 cites W2067570815 @default.
- W2147003679 cites W2067989729 @default.
- W2147003679 cites W2068403951 @default.
- W2147003679 cites W2070148075 @default.
- W2147003679 cites W2073097483 @default.
- W2147003679 cites W2090083374 @default.
- W2147003679 cites W2090206242 @default.
- W2147003679 cites W2093317589 @default.
- W2147003679 cites W2119247793 @default.
- W2147003679 cites W2132746247 @default.
- W2147003679 cites W2138522501 @default.
- W2147003679 cites W2169072530 @default.
- W2147003679 cites W2248650298 @default.
- W2147003679 cites W2332647243 @default.
- W2147003679 cites W4254876612 @default.
- W2147003679 cites W571041058 @default.
- W2147003679 doi "https://doi.org/10.1111/iar.12086" @default.
- W2147003679 hasPublicationYear "2014" @default.
- W2147003679 type Work @default.
- W2147003679 sameAs 2147003679 @default.
- W2147003679 citedByCount "15" @default.
- W2147003679 countsByYear W21470036792014 @default.
- W2147003679 countsByYear W21470036792017 @default.
- W2147003679 countsByYear W21470036792018 @default.
- W2147003679 countsByYear W21470036792019 @default.
- W2147003679 countsByYear W21470036792020 @default.
- W2147003679 countsByYear W21470036792022 @default.
- W2147003679 crossrefType "journal-article" @default.
- W2147003679 hasAuthorship W2147003679A5000130543 @default.
- W2147003679 hasAuthorship W2147003679A5004999383 @default.
- W2147003679 hasAuthorship W2147003679A5010757634 @default.
- W2147003679 hasAuthorship W2147003679A5047092458 @default.
- W2147003679 hasAuthorship W2147003679A5049038755 @default.
- W2147003679 hasAuthorship W2147003679A5054097438 @default.
- W2147003679 hasAuthorship W2147003679A5054419460 @default.
- W2147003679 hasAuthorship W2147003679A5054716335 @default.
- W2147003679 hasAuthorship W2147003679A5071225732 @default.
- W2147003679 hasConcept C127313418 @default.
- W2147003679 hasConcept C161509811 @default.
- W2147003679 hasConcept C167919410 @default.
- W2147003679 hasConcept C17409809 @default.
- W2147003679 hasConcept C26687426 @default.
- W2147003679 hasConcept C2777640183 @default.
- W2147003679 hasConcept C2778849375 @default.
- W2147003679 hasConcept C2780040746 @default.
- W2147003679 hasConcept C67236022 @default.
- W2147003679 hasConcept C79572550 @default.
- W2147003679 hasConceptScore W2147003679C127313418 @default.
- W2147003679 hasConceptScore W2147003679C161509811 @default.
- W2147003679 hasConceptScore W2147003679C167919410 @default.
- W2147003679 hasConceptScore W2147003679C17409809 @default.
- W2147003679 hasConceptScore W2147003679C26687426 @default.
- W2147003679 hasConceptScore W2147003679C2777640183 @default.
- W2147003679 hasConceptScore W2147003679C2778849375 @default.
- W2147003679 hasConceptScore W2147003679C2780040746 @default.