“…Lazarov et al, 2009Lazarov et al, , 2012Shu et al, 2013), T RD and T MA Re-Os model ages of peridotites and sulfides, and sulfide Re-Os isochrons Richardson et al, 1984;Pearson et al, 1995;Jacob et al, 1998) and garnet inclusions in diamonds (= diamonds from Richardson et al, 1984;Richardson and Harris, 1997) in a εNd (0) versus 147 Sm/ 144 Nd diagram. This kind of "isochron" diagram shows (i) the very negative εNd (0) that are common to subcalcic garnet xenocrysts and garnet inclusions in diamonds, (ii) that multiple overprints affected the majority of the subcalcic garnets (large spread to less negative and positive εNd) whereas the inclusions have only negative values and (iii) reliable age information may be obtained only from individual localities.…”