Fig. 5: Boron and radiogenic isotopes and trace element systematics of the ELIP rock samples.
From: Heavy boron isotopes in plume-derived magmas trace recycled water in deep-mantle reservoir
Plots of a δ11B, b 143Nd/144Nd, c 87Sr/86Sr, and d B/Ce vs. La/Yb for the ELIP picrites and basalts. The B/Ce ratios of the olivine-hosted melt inclusions in the picrite sample are plotted for comparison. “High-F melt, refractory lithologies” refer to a high fraction of melts from more refractory and depleted lithologies in the mantle source. “Low-F melt, fusible lithologies” refers to a low fraction of melts from more fusible and enriched lithologies in the mantle source. The literature data for the ELIP picrites and basalts for comparison in b are compiled from the database GEOROC.
