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

Abstract 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 extensiv...

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Autores principales: Costanza Bonadiman, Valentina Brombin, Giovanni B. Andreozzi, Piera Benna, Massimo Coltorti, Nadia Curetti, Barbara Faccini, Marcello Merli, Beatrice Pelorosso, Vincenzo Stagno, Magdala Tesauro, Alessandro Pavese
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/840c784f6ced414882045257231e3c6a
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