“…Therefore, pyrite can preserve information about the original formation of the sulfides. Trace element compositions of pyrite have been used as genetic fingerprints (e.g., Loftus-Hills and Solomon, 1967); for example, Co/Ni ratios can be used as an empirical indicator of the formation the environment of pyrite (e.g., Davidson, 1962;Loftus-Hills and Solomon, 1967;Bralia et al, 1979;Ivor Roberts, 1982;Bajwah et al, 1987;Raymond, 1996;Craig et al, 1998;Clark et al, 2004;Koglin et al, 2010;Ulrich et al, 2011;Winderbaum et al, 2012). However, the use of this ratio needs to take into account other provenance factors, as obtained from field observations and other data.…”