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- W2214976465 abstract "Zn-Pb-Fe ores in the Ali ou Daoud deposit (Central High Atlas) are found as stratiform levels and as karst fillings in carbonate platforms facies of Bajocian age. Tectonic structures (e.g., synsedimentary faults) played a relevant role in the ore emplacement. The dolomitic ore-related host-rock levels are characterized by the presence of kaolinite enrichment in clay levels in amounts directly related to the proportion of the clay minerals. The latter is evidenced by correlation between kaolinite and sulphide contents, suggesting that the installation of kaolinite and mineralisations would result from the same hydrothermal fluid." @default.
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- W2214976465 date "2008-10-22" @default.
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- W2214976465 title "Pb-Zn mineralization of Ali ou Daoud area (Central High Atlas, Morocco): characterisation of deposit and relationships with the clay assemblages" @default.
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- W2214976465 doi "https://doi.org/10.3989/egeol.08642.038" @default.
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