Extreme geochemical variability through the dunitic transition zone of the Oman ophiolite: Implications for melt/fluid-rock reactions at Moho level beneath oceanic spreading centers-Reference-Cited by-同舟云学术

Extreme geochemical variability through the dunitic transition zone of the Oman ophiolite: Implications for melt/fluid-rock reactions at Moho level beneath oceanic spreading centers

Published:2018-08 Issue: Volume:234 Page:1-23
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Rospabé Mathieu,Benoit Mathieu,Ceuleneer Georges,Hodel Florent,Kaczmarek Mary-Alix

Funder

Centre National de la Recherche Scientifique-Institut National des Sciences de l’Univers – France

Swiss National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference139 articles.

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3. High-temperature hydrothermal activities around suboceanic Moho: an example from diopsidite and anorthosite in Wadi Fizh, Oman ophiolite;Akizawa;Lithos,2016

4. An estimation of the least depleted spinel peridotite on the basis of olivine-spinel mantle array;Arai;Neues Jahrb. für Mineral. - Monatshefte,1987

5. Characterization of spinel peridotites by olivine-spinel compositional relationships: review and interpretation;Arai;Chem. Geol.,1994

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