Hydrated Peridotite – Basaltic Melt Interaction Part I: Planetary Felsic Crust Formation at Shallow Depth

Hydrated Peridotite – Basaltic Melt Interaction Part I: Planetary Felsic Crust Formation at Shallow Depth

Current theories suggest that the first continental crust on Earth, and possibly on other terrestrial planets, may have been produced early in their history by direct melting of hydrated peridotite. However, the conditions, mechanisms and necessary ingredients for this crustal formation remain elusi...

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Bibliographic Details
Main Authors: Anastassia Y. Borisova, Nail R. Zagrtdenov, Michael J. Toplis, Wendy A. Bohrson, Anne Nédélec, Oleg G. Safonov, Gleb S. Pokrovski, Georges Ceuleneer, Ilya N. Bindeman, Oleg E. Melnik, Klaus Peter Jochum, Brigitte Stoll, Ulrike Weis, Andrew Y. Bychkov, Andrey A. Gurenko, Svyatoslav Shcheka, Artem Terehin, Vladimir M. Polukeev, Dmitry A. Varlamov, Kouassi Chariteiro, Sophie Gouy, Philippe de Parseval
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Earth Science
Subjects:
experiment
basaltic melt-serpentinite rock interaction
TTG
ophiolites
Hadean eon
Noachian
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.640464/full

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https://www.frontiersin.org/articles/10.3389/feart.2021.640464/full

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