Amphibolization of MG-and FE-rich gabbroic dykes within mantle-derived serpentinites from northern Apennine ophiolites evidence for high-temperature hydration of the oceanic lithosphere
R. Tribuzio et al., Amphibolization of MG-and FE-rich gabbroic dykes within mantle-derived serpentinites from northern Apennine ophiolites evidence for high-temperature hydration of the oceanic lithosphere, Ofioliti (Bologna) Bollettino del gruppo di lavoro sulle ofioliti mediterranee , 22(1), 1997, pp. 71-79