Iron isotopic fractionation between silicate mantle and metallic core at high pressure

The +0.1‰ elevated (56)Fe/(54)Fe ratio of terrestrial basalts relative to chondrites was proposed to be a fingerprint of core-mantle segregation. However, the extent of iron isotopic fractionation between molten metal and silicate under high pressure–temperature conditions is poorly known. Here we s...

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Detalles Bibliográficos
Autores principales: Liu, Jin, Dauphas, Nicolas, Roskosz, Mathieu, Hu, Michael Y., Yang, Hong, Bi, Wenli, Zhao, Jiyong, Alp, Esen E., Hu, Justin Y., Lin, Jung-Fu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5321738/
https://www.ncbi.nlm.nih.gov/pubmed/28216664
http://dx.doi.org/10.1038/ncomms14377

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5321738/
https://www.ncbi.nlm.nih.gov/pubmed/28216664
http://dx.doi.org/10.1038/ncomms14377

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