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Minerals, Volume 15, Issue 3
March 2025 - 132 articles
Cover Story: The Walton carbonate-replacement Ag-Pb-Zn-Cu sulphide deposit consists of a finely crystalline massive baryte body overlying a siderostone-hosted sulphide body. The siderostone formed due to dissimilatory iron reduction (DIR) that led to the breakdown of Fe–Mn oxyhydroxides and organic matter, whereas the massive baryte body likely resulted from the mixing of sulphate-rich and Ba-rich fluid reservoirs. Siderite and baryte are abundant in many sedimentary rock-hosted sulphide deposits; therefore, their origin is essential to understanding the genesis of the deposit. View this paper
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Minerals - ISSN 2075-163X