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Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: Major element composition of an Early Enriched Reservoir: constraints from 142Nd/144Nd isotope systematics in the early Earth and high-pressure melting experiments of a primitive peridotite

Fig. 5

Comparison of the major element compositions of the 1, 3, and 7 GPa near-solidus melts (Falloon et al. 2008; Davis et al. 2011; this study) with the 3.3–3.5 Ga Barberton komatiites (Robin-Popieul et al. 2012), 2.7 Ga Abitibi komatiites (Kerrich and Xie 2002), and 3.8 Ga Isua MORB and OIB (Komiya et al. 2004). MORB mid-ocean ridge basalt, OIB ocean island basalt

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