Fe-Ti-Zr metasomatism in the oceanic mantle due to extreme differentiation of tholeiitic melts (Moa-Baracoa ophiolite, Cuba)-Reference-Cited by-同舟云学术

Fe-Ti-Zr metasomatism in the oceanic mantle due to extreme differentiation of tholeiitic melts (Moa-Baracoa ophiolite, Cuba)

Published:2020-04 Issue: Volume:358-359 Page:105420
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Pujol-Solà Núria,Proenza Joaquín A.,Garcia-Casco Antonio,González-Jiménez José María,Román-Alpiste Manuel J.,Garrido Carlos J.,Melgarejo Joan Carles,Gervilla Fernando,Llovet Xavier

Funder

Spanish Project

Spanish “Ministerio de Economía y Competitividad”

“Ministerio de Ciencia, Innovación y Universidades”

Ramón y Cajal Fellowship

Ministerio de Educación

University of Granada

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference164 articles.

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3. Formation and modification of chromitites in the mantle;Arai;Lithos,2016

4. Zircon coronas around Fe–Ti oxides: a physical reference frame for metamorphic and metasomatic reactions;Austrheim;Contrib. Mineral. Petrol.,2008

5. Zr-and Ba-rich minerals from the Ponte Nova alkaline mafic-ultramafic massif, southeastern Brazil: indication of an enriched mantle source;Azzone;Can. Mineral.,2009

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