“…A crucial point for the use of Fe isotopes to trace ancient metals is the isotopic variability of the ore sources. Many authors investigated the fractionation processes of Fe isotopes in magmatic and hydrothermal systems (e.g., Bilenker et al, 2016;Gagnevin et al, 2012;Günther et al, 2017;Sun et al, 2013;Wang et al, 2011;Zhao et al, 2019) or in sedimentary iron ores (e.g., Busigny & Dauphas, 2007;Czaja et al, 2013;Halverson et al, 2011;Rose et al, 2019). In high-temperature magmatic and hydrothermal systems, Fe isotope fractionation may occur between early crystallizing Fe minerals and the residual magma or hydrothermal fluid (e.g., Gagnevin et al, 2012;Wang et al, 2011Wang et al, , 2015Zhao et al, 2019).…”