Definition
The term chalcophile (derived from the Greek for copper-loving) was originally introduced by Goldschmidt (1923) to describe the group of elements that are concentrated in sulfide minerals in meteorites. Traditionally this group is defined as the elements Ag, As, Bi, Cd, Cu, Hg, In, Pb, S, Sb, Se, Te, Tl, and Zn. Goldschmidt classified the other elements in meteorites into two groups: those associated with Fe alloy as siderophile (iron loving) and those concentrated in silicates minerals as lithophile (rock loving). Subsequently Goldschmidt applied his classification to the whole Earth and modified it to include two new groups of elements: atmophile, those concentrated in the atmosphere and biophile elements, those concentrated by organic processes (Goldschmidt 1930).
Distribution in Terrestrial Rocks
Whereas the concepts outlined by Goldschmidt are useful, as is evidenced by the fact the terms, siderophile, chalcophile, and lithophile are in daily use by geochemists, the...
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Barnes, SJ. (2018). Chalcophile Elements. In: White, W.M. (eds) Encyclopedia of Geochemistry. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-39312-4_220
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