Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite

Here we show how the Higashi-akaishi peridotite body in the Sanbagawa metamorphic belt, a sliver of the former mantle wedge of the eastern Eurasian plate margin, has exhumed subduction fluid noble gases and halogens with a marine pore-fluid signature from a depth of ~ 100. km. Previous work has only...

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Библиографические подробности
Главные авторы: Sumino, H, Burgess, R, Mizukami, T, Wallis, SR, Holland, G, Ballentine, C
Формат: Journal article
Язык:English
Опубликовано: 2010