Fig. 15
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Th/Yb vs. Ta/Yb diagram from Pearce (1983, 2008) showing the mafic rocks studied in this work and those reported for the CIZ and the Armorican Massif. The rocks from CS show a less enriched and less metasomatized mantle source compared to the rocks from AS and GS. The CS is consistent with the data reported for the Armorican Massif (Pochon et al., 2016b). References in the figure: 1(Orejana et al., 2009); 2(Scarrow et al., 2009); 3(López-Moro et al., 2007); 4(Pochon et al., 2016b).
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