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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...
Autores principales: | , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2019
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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 |