WebApr 1, 1996 · Dans les bassins de l'Oued Zat et Ida Ou Zal, sur le socle paléozoïque, reposent des formations détritiques continentales d'âge stéphanien supérieur. L'analyse des structures tectono-sédimentaires confirme le contrôle de la sédimentation par des accidents affectant le substratum, dans un régime extensif de direction nordouest-sudest à est-ouest. </a>

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