Comments on the paper Ti-poor high-Al chromitites of the Moa-Baracoa ophiolitic massif (eastern Cuba) formed in a nascent forearc mantle by Rui et al. [ore Geol. Rev., 104847]
Diamond forms during low pressure serpentinisation of oceanic lithosphere
Authors: Pujol-Sola, N.; Garcia-Casco, A.; Proenza, J. A.; Gonzalez-Jimenez, J. M.; del Campo, A.; Colas, V; Canals, A.; Sanchez-Navas, A.; Roque-Rosell, J.