Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa - a potential mechanism for diamond formation during subduction - Archive ouverte HAL
Article Dans Une Revue European Journal of Mineralogy Année : 2011

Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa - a potential mechanism for diamond formation during subduction

Audrey Martin
Laboratoire Magmas et Volcans
NASA Johnson Space Center
Tahar Hammouda
Laboratoire Magmas et Volcans
CV

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Sylvaine Jouhannel  : Connectez-vous pour contacter le contributeur

https://hal.science/hal-00682692

Soumis le : lundi 26 mars 2012-15:05:59

Dernière modification le : lundi 2 décembre 2024-14:48:10

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hal-00682692 , version 1 (26-03-2012)

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Audrey Martin, Tahar Hammouda. Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa - a potential mechanism for diamond formation during subduction. European Journal of Mineralogy, 2011, 23, pp.5-16. ⟨10.1127/0935-1221/2010/0022-2067⟩. ⟨hal-00682692⟩

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