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The proposed metallogenetic model presented in this paper is based on observations from the Iranian non-sulphide zinc deposits Mehdi-Abad, Iran-Kuh, and Kuh-e-Surmeh. The emplacement of non-sulphide ore can be generally subdivided into an ‘oxidation stage’ followed by a ‘post-oxidation stage’. The formation of carbonate-hosted non-sulphide zinc deposits is primarily controlled by three factors: climate,...
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