Abstract:The tectonic and microtectonic analysis of the Paleozoic and MesoCenozoic series of the Bouchfâa zone (NW of Tazekka) enabled us to highlight tectonic palaeo-stress of essentially compressive stresses. These played a key role in the uprising of the Tazekka Massif. The age and chronology of these paleo-stress are established by analogy with the results obtained in the Middle Atlas, Saïs and High Moulouya. The N165 major compressive phase of post-Bathonian and ante-Barremianage, responsible for the thrust of Low… Show more
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