Hydrated Peridotite–Basaltic Melt Interaction Part II: Fast Assimilation of Serpentinized Mantle by Basaltic Magma

The most abundant terrestrial lavas, mid-ocean ridge basalt (MORB) and ocean island basalt (OIB), are commonly considered to be derived from a depleted MORB-mantle component (DMM) and more specific, variably enriched mantle plume sources. However, findings of oceanic lavas and mafic cumulates issued...

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Autores principales:	Anastassia Y. Borisova, Nail R. Zagrtdenov, Michael J. Toplis, Georges Ceuleneer, Oleg G. Safonov, Gleb S. Pokrovski, Klaus Peter Jochum, Brigitte Stoll, Ulrike Weis, Svyatoslav Shcheka, Andrey Y. Bychkov
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	Frontiers Media S.A. 2020-04-01
Colección:	Frontiers in Earth Science
Materias:	hydrated peridotite serpentinite basaltic melt assimilation MORB melt–rock interaction
Acceso en línea:	https://www.frontiersin.org/article/10.3389/feart.2020.00084/full
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