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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...
Uloženo v:
| Vydáno v: | Sci Adv |
|---|---|
| Hlavní autoři: | , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American Association for the Advancement of Science
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6920019/ https://ncbi.nlm.nih.gov/pubmed/31897427 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aax8648 |
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