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Fluid inclusion and stable isotope data on the Palaeozoic basement-hosted Peyrebrune (Zn, F) Iode-deposit (Albigeois region), indicate that mineralization originated from circulation of basinal-derived brines during distinct successive Mesozoic extensional events. These new data, set in a regional context, suggest the occurrence of two distinct evaporite-bearing sedimentary basins, now concealed...
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