Evidence for isotopically light Fe mobility under oxidising conditions in subduction zone fluids: A record of Monviso meta-serpentinites, Western Alps-Reference-Cited by-同舟云学术

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Evidence for isotopically light Fe mobility under oxidising conditions in subduction zone fluids: A record of Monviso meta-serpentinites, Western Alps

Published:2024-09 Issue: Volume:642 Page:118855
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Debret Baptiste^ORCID,Caurant Clara,Ménez Bénédicte,Busigny Vincent^ORCID,Moynier Frédéric

Publisher

Elsevier BV

Reference87 articles.

1. Subduction of oceanic lithosphere in the Alps: selective and archetypal from (slow-spreading) oceans;Agard;Earth-Science Rev.,2021

2. Tectonometamorphic evolution of the schistes lustres complex; implications for the exhumation of HP and UHP rocks in the Western Alps;Agard;Bull. la Société géologique Fr.,2001

3. Determination of ferrous iron in non-refractory silicate minerals. 1. An improved semi-micro oxidimetric method;Amonette;Chem. Geol.,1991

4. Subduction interface processes recorded by eclogite-facies shear zones (Monviso, W. Alps);Angiboust;Lithos,2011

5. Eclogitization of the Monviso ophiolite (W. Alps) and implications on subduction dynamics;Angiboust;J. Metamorph. Geol.,2012

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