Abstract
In the F53 Aït Ahmane Cobalt-deposit (Bou Azzer, Anti-Atlas, Morocco) a new type of “contact mineralization” is described. It is carbonate hosted but displays similar depositional sequence and fluid inclusion patterns to the well-known vein mineralization from the same mine. Field studies suggest that such a “contact mineralization” formed early by infilling solution cavities in formerly calcified serpentinite.
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Ennaciri, A., Barbanson, L. & Touray, J.C. Mineralized hydrothermal solution cavities in the Co-As Aït Ahmane mine (Bou Azzer, Morocco). Mineral. Deposita 30, 75–77 (1995). https://doi.org/10.1007/BF00208879
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DOI: https://doi.org/10.1007/BF00208879