formations of the Saghro inlier (eastern part of the Anti-Atlas Mountains, Morocco). The
orebodies consist of northeast-southwest to east-west veins and lenses hosted by
Cryogenian black shales and gray-wackes and Neoproterozoic conglomerates, and are
controlled by an east-west fault network, the so-called Imiter fault. Mineralogical and paleo-
fluid geochemistry investigations (microthermometry, Raman spectroscopy, LA-ICP-MS on …