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 Accéder directement au contenu
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

Tahar Hammouda
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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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