Articles | Volume 17, issue 9
https://doi.org/10.5194/se-17-1063-2026
https://doi.org/10.5194/se-17-1063-2026
Research article
 | 
21 Sep 2026
Research article |  | 21 Sep 2026

Petrogenesis and geodynamic setting of Ediacaran rocks from the Sirwa massif, Central Anti-Atlas of Morocco

Abdelhay Ben-Tami, Saïd Belkacim, Jamal El Kabouri, Bouchra Baidada, Joshua H. F. L. Davies, Morgann G. Perrot, Mohamed Bhilisse, Mohamed Assalmi, Mariam Ferraq, and Mohamed Bouabdellah

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Cited articles

Abati, J., Aghzer, A. M., Gerdes, A., and Ennih, N.: Detrital zircon ages of Neoproterozoic sequences of the Moroccan Anti-Atlas belt, Precambrian Res., 181, 115–128, https://doi.org/10.1016/j.precamres.2010.05.018, 2010. 
Admou, H., Fekkak, A., Razin, P., Egal, E., Youbi, N., Soulaimani, A., Blein, O., Baudin, T., and Chevremont, P.: Carte géologique Maroc (1/50000), feuille d'Aït Ahmane, Notes et Mémoires Service Géologique Maroc, no. 533, 2013. 
Aït Malek, A., Gasquet, D., Bertrand, J. M., and Leterrier, J.: Géochronologie U-Pb sur zircon de granitoïdes éburnéens et panafricains dans les boutonnières protérozoïques d'Igherm, du Kerdous et du Bas Drâa (Anti-Atlas occidental, Maroc), C. R. Acad. Sci. IIA–Earth and Planetary Science, 327, 819–826, https://doi.org/10.1016/S1251-8050(99)80056-1, 1998. 
Álvaro, J. J., Benziane, F., Thomas, R., Walsh, G. J., and Yazidi, A.: Neoproterozoic–Cambrian stratigraphic framework of the Anti–Atlas and Ouzellagh promontory (High Atlas), Morocco, J. Afr. Earth Sci., 98, 19–33, https://doi.org/10.1016/j.jafrearsci.2014.04.026, 2014a. 
Álvaro, J. J., Pouclet, A., Ezzouhairi, H., Soulaimani, A., Bouougri, E. H., Imaz, A. G., and Fekkak, A.: Early Neoproterozoic rift-related magmatism in the Anti-Atlas margin of the West African craton, Morocco, Precambrian Res., 255, 433–442, https://doi.org/10.1016/j.precamres.2014.10.008, 2014b. 
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Short summary
Detrital zircons from Saghro Group sediments reveal the underlying basement's nature within the Sirwa massif. The returned 2.1 Ga age indicates Paleoproterozoic basement exposure along the Saghro Group basin margins, without Ediacaran sediment interaction. These findings support the hypothesis of Paleoproterozoic crust extending north of the Anti-Atlas Major Fault (AAMF), suggesting a definitive suture zone may extend further north, possibly aligning with the South Atlas Fault (SAF).
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