Skip to main content

Advertisement

Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

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. 7

Densities of the solidus melt and mantle peridotite at 1, 3, and 7 GPa. Diamonds and rectangles show densities of the primitive peridotite and densities of the near-solidus melts, respectively. The solidus melts are less dense than the mantle peridotite. Therefore, the solidus melts should ascend in the mantle

Back to article page