is there a relationship between the copper mineralization hosted in the Neoproterozoic basement formations and the other that is hosted in the Cambrian cover in all the inliers (Boutonnières) of the Moroccan Anti Atlas ?
It is possible that the ore hosted in the Neoproterozoic can be remobilized by the deep-seated fluids which would carry the metals to the Cambrian site where they can be redeposited. Beside geologic and tectonic data, geochemical analysis can be performed to find if any genetic relationship exist between the copper mineralization hosted in the basement and its cover.
Relationship between the copper mineralization hosted in the Neoproterozoic basement formations and the other that is hosted in the Cambrian cover perhaps can be proven with compared fluid caracterisation in host rock and basement formations.