Trace element substitution and grain-scale compositional heterogeneity in enargite
Abstract
Enargite, Cu3AsS4, is a relatively common sulphide mineral and is considered diagnostic for deposits of intermediate- to high-sulphidation type. Analysis of enargite-bearing samples from deposits in the Zijinshan porphyry – high-sulphidation epithermal Cu-Au orefield, southeastern China, provides evidence for the diversity of trace elements that may be hosted within enargite and their range of concentrations. Enargite is shown to host Sb, Te,...
Paper Details
Title
Trace element substitution and grain-scale compositional heterogeneity in enargite
Published Date
Aug 1, 2019
Journal
Volume
111
Pages
103004 - 103004
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