Figure 2: Behaviour of H2O and Cl in the equatorial MAR melt inclusions.
From: Heterogeneity in mantle carbon content from CO2-undersaturated basalts
(a) Variation in H2O content (wt%) as a function of Ce content (p.p.m.) for the equatorial MAR melt inclusions and matrix glasses. (b) Variation in Cl content (p.p.m.) as a function of Nb content (p.p.m.) for the equatorial melt inclusions and matrix glasses.
