“…Documentation of the spatial heterogeneity of ancient silver has been demonstrated for S, Cu, and Bi in metal grains, and silicon oxide and iron oxide inclusions have been documented, particularly in primary (non-remelted and re-cast) metal (Giovannelli et al , 2005). Similarly, Fe, Zn, Au, Hg, and Pb have been shown to exhibit spatial variability at scales of 0.02–0.2 mm (Uzonyi et al , 2000, their Fig. 3; Kantarelou et al , 2011).…”