Fig. 3: Whole-rock δ65Cu and Cu content correlations with geochemical proxies constraining magmatic processes in the Emeishan lavas.
From: Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
Whole-rock Cu versus Pd (a), and δ65Cu versus Mg# (b), Cr (c), V/Sc (d), ƐNd(t) (e), and 105 × Pd/Yb (f). Compositions of end-members for binary mixing model are listed in Supplementary Data 2. Error bars are 2 SD.
