Planetary Felsic Crust Formation at Shallow Depth

Current theories suggest that on Earth and, possibly, on other terrestrial planets early in their history, the first continental crust may has been produced by direct melting of hydrated peridotite. However, the conditions, mechanisms and necessary ingredients of such production remain elusive. To f...

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Veröffentlicht in:	arXiv.org 2020-03
Hauptverfasser:	Borisova, Anastassia Y, Zagrtdenov, Nail R, Toplis, Michael J, Bohrson, Wendy A, Nedelec, Anne, Safonov, Oleg G, Pokrovski, Gleb S, Ceuleneer, Georges, Bindeman, Ilya N, Melnik, Oleg E, Jochum, Klaus Peter, Stoll, Brigitte, Weis, Ulrike, Bychkov, Andrew Y, Gurenko, Andrey A, Shcheka, Svyatoslav, Terehin, Artem, Polukeev, Vladimir M, Varlamov, Dmitry A, Kouassi E A Chariteiro, Gouy, Sophie, De Parseval, Philippe
Format:	Artikel
Sprache:	eng
Schlagworte:	Asthenosphere Direct melting Earth crust Embryos Lithosphere Magma Peridotite Planet formation Plate tectonics Silicon dioxide Solidification Terrestrial planets
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