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Gradual and selective trace-element enrichment in slab-released fluids at sub-arc depths
The geochemical signature of magmas generated at convergent margins greatly depends on the nature of fluids and melts released during subduction. While major- and trace-elements transport capacity of ultrahigh pressure (UHP) hydrous-silicate melts has been investigated, little is known about solute...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6841933/ https://www.ncbi.nlm.nih.gov/pubmed/31704982 http://dx.doi.org/10.1038/s41598-019-52755-9 |