Figure 6
From: Genesis of ultra-high-Ni olivine in high-Mg andesite lava triggered by seamount subduction
Mineral compositions of the EC lavas. (a) Cr# in Sp vs. Fo diagram. Mantle array (OSMA)29 shown by two dashed lines. (b) Ni abundance of Cpx in the HMA and B. Gray dashed line indicates fractional crystallization trend of Ol and Cpx and solid gray line indicates olivine fractional crystallization trend from primitive melt, as in Fig. 5b. Colors represent each rock type as identified in Fig. 2.
