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- W2016125004 abstract "La découverte de Saccogonum cf. saccatum, Brachiopodedu Cambrien (supérieur?), dans le massif ancien du Haut-Atlas occidental entre la zone faillée Aït Lahsen-Talmakent et le granite du Tichka permet de dater ces terrains, épimétamorphiques, de l'intervalle Cambrien inférieur à Ordovicien inférieur. Les corrélations qui en découlent dans le Haut-Atlas occidental montrent que la zone faillée évoquée était individualsée au Cambrien moyen. A l'échelle du Maroc, le Cambrien supérieur correspond à une période de surrection accompagnée d'une érosion intense responsable de la quasi absence de sédiments de cet âge. Discovery of Saccogonum cf. saccatum (Upper?)Cambrian brachiopod, in the Paleozoic Western High Atlas between the Aït Lahsen Talmakent fault and the Tichka granite shows that the age of these epimetamorphic rocks ranges from Lower Cambrian to Lower Ordovician. Correlations in the western Atlas suggest that the Aït Lahsen-Talmakent fault was yet active during Middle Cambrian. In Morocco, Upper Cambrian is characterized by epeïrogenic movements with strong erosion, so that sedimentary rocks of this age are seldom preserved." @default.
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- W2016125004 title "Découverte de Saccogonum cf. Saccatum, Brachiopode duCambrien (Supérieur?), dans le Haut-Atlas occidental (Maroc). Conséquences stratigraphiques et structurales" @default.
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