Phlogopite-pargasite coexistence in an oxygen reduced spinel-peridotite ambient

The occurrence of phlogopite and amphibole in mantle ultramafic rocks is widely accepted as the modal effect of metasomatism in the upper mantle. However, their simultaneous formation during metasomatic events and the related sub-solidus equilibrium with the peridotite has not been extensively studi...

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Detalles Bibliográficos
Autores principales: Bonadiman, Costanza, Brombin, Valentina, Andreozzi, Giovanni B., Benna, Piera, Coltorti, Massimo, Curetti, Nadia, Faccini, Barbara, Merli, Marcello, Pelorosso, Beatrice, Stagno, Vincenzo, Tesauro, Magdala, Pavese, Alessandro
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8178368/
https://www.ncbi.nlm.nih.gov/pubmed/34088914
http://dx.doi.org/10.1038/s41598-021-90844-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8178368/
https://www.ncbi.nlm.nih.gov/pubmed/34088914
http://dx.doi.org/10.1038/s41598-021-90844-w

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