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Article Dans Une Revue Geochimica et Cosmochimica Acta Année : 2022

Stable isotope geochemistry of silicon in granitoid zircon

Résumé

Zircon is often used to study granites (sensu lato) and continental crust because it is very resistant and can be analyzed for various isotope systems that provide time and source information about their parental melts. Granites with different petrological histories have distinct bulk-rock silicon isotope compositions but it is unclear if these differences are also detectable in zircon because of superimposed fractionation effects (e.g., related to temperature, silica content, magmatic processes). The present study explores the Si isotope signatures of zircon from various granite types to constrain their isotope fractionation behavior and uses Revised Manuscript-Clean Click here to view linked References

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Géochimie
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Dates et versions

hal-03516880 , version 1 (19-01-2022)

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Paternité - Pas d'utilisation commerciale - Pas de modification

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Martin Guitreau, Abdelmouhcine Gannoun, Zhengbin Deng, Marc Chaussidon, Frédéric Moynier, et al.. Stable isotope geochemistry of silicon in granitoid zircon. Geochimica et Cosmochimica Acta, 2022, 316, pp.273-294. ⟨10.1016/j.gca.2021.09.029⟩. ⟨hal-03516880⟩
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