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Extreme Zr stable isotope fractionation during magmatic fractional crystallization

Zirconium is a commonly used elemental tracer of silicate differentiation, yet its stable isotope systematics remain poorly known. Accessory phases rich in Zr(4+) such as zircon and baddeleyite may preserve a unique record of Zr isotope behavior in magmatic environments, acting both as potential dri...

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Detalles Bibliográficos
Autores principales: Ibañez-Mejia, Mauricio, Tissot, François L. H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6920019/
https://www.ncbi.nlm.nih.gov/pubmed/31897427
http://dx.doi.org/10.1126/sciadv.aax8648