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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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| Pubblicato in: | Nat Commun |
|---|---|
| Autori principali: | , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2019
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6325133/ https://ncbi.nlm.nih.gov/pubmed/30622301 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-08001-3 |
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