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Minerals, Volume 8, Issue 2
February 2018 - 46 articles
Cover Story: We show that the Fe-Mn-Cu ore deposit of Jbel Rhals (Morocco) has a polyphased metallogenic history, with mineralization resulting from supergene processes superimposed over hydrothermal alteration. Weathering most probably related to the Cenozoic uplift(s) of the High Atlas enabled the formation of a supergene ore mainly composed of goethite replacing, by pseudomorphose, hydrothermal siderite. The supergene processes also led to an enrichment in HREE, Y, and mobile elements such as U in secondary minerals. View this paper
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Minerals - ISSN 2075-163X