Sulfide resorption during crustal ascent and degassing of oceanic plateau basalts

Mantle plume-related magmas typically have higher chalcophile and siderophile element (CSE) contents than mid-ocean ridge basalts (MORB). These differences are often attributed to sulfide-under-saturation of plume-related melts. However, because of eruption-related degassing of sulfur (S) and the co...

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Detalles Bibliográficos
Autores principales: Reekie, C. D. J., Jenner, F. E., Smythe, D. J., Hauri, E. H., Bullock, E. S., Williams, H. M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6325133/
https://www.ncbi.nlm.nih.gov/pubmed/30622301
http://dx.doi.org/10.1038/s41467-018-08001-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6325133/
https://www.ncbi.nlm.nih.gov/pubmed/30622301
http://dx.doi.org/10.1038/s41467-018-08001-3

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