Fig. 2: Chemical variations due to magmatic evolution to form Pagan and NW Rota-1 volcanic rocks. | Nature Communications

Fig. 2: Chemical variations due to magmatic evolution to form Pagan and NW Rota-1 volcanic rocks.

From: Molybdenum isotopes unmask slab dehydration and melting beneath the Mariana arc

Fig. 2

Plots of a Mo, b Dy/Yb, c Ce/Mo, and d δ98/95Mo vs. MgO diagrams for the Pagan and NW Rota-1 samples. COB clinopyroxene-olivine basalt, POB plagioclase-olivine basalt, SD standard deviation, which is based on duplicate analyses of standard solution NIST SRM 3134, reference materials AGV-2 and W-2a, IAPSO seawater standard, and unknown samples.

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