From the hercynian orogenic cycle towards the central atlantic prerifting in morocco: is the central swarm of lamprophyric dykes and sills a possible magmatic marker for this transition?
Auteur
Aarab E.M. Boumehdi My A. Youbi N. Bensalah M.K. Assafar H., Ben Abbou M., Rkha Chaham K
Manifestation
9ème Colloque international International Magmatisme Métamorphisme et Minéralisations Associées (3MA)
