Fig. 1: The whole-rock δ65Cu values of the Emeishan lavas in comparison with peridotites, basalts, and other geological reservoirs reported in literatures.
From: Copper isotope evidence for recycled crustal sulfides in deep mantle plume source
Fig. 1: The whole-rock δ65Cu values of the Emeishan lavas in comparison with peridotites, basalts, and other geological reservoirs reported in literatures. | Communications Earth & Environment
