The Imiter inlier (eastern part of the Moroccan Anti-Atlas) is located on the northwestern border of the West African Craton (WAC) and exhibits a range of Pan-African granitoids. Three massifs that crosscut the Imiter Saghro Group were targeted in this work: the Igoudrane granodiorite, Bou Teglimt granodiorite and Bou Fliou granite. We present here additional geochemical analyses (major and trace elements) and Sm-Nd isotopic data, which define two distinct groups: (i) the Igoudrane massif (677 Ma) and (ii) the Bou Teglimt granodiorite (576 Ma) and the Bou Fliou granite (550 Ma).Geochemical data confirm the calc-alkaline signature of the studied granitoids. Both groups of granitoids are slightly peraluminous and show strong negative anomalies in Nb, Ta and Ti in multi-element plots normalized to the primitive mantle. The granitoids have low 143Nd/144Nd initial ratios (0.5116-0.5117), with TDM model ages ranging from 1.73 to 1.52Ga. The ╬ÁNd(t) values are negative, decreasing from the Igoudrane samples (-1.1 to -3.1) to the Bou Teglimt granodiorite (-3.0 to -3.3) and Bou Fliou (-4.2 to -4.8). All these data suggest a mixed magmatic origin involving a juvenile mantle source and an old, at least Paleoproterozoic crust. Given Mesoproterozoic rocks are lacking or very scarce in the Anti-Atlas, these results confirm the existence of an old cratonic basement beneath the eastern Anti-Atlas, and therefore suggest that the northern border of the West African Craton must be placed further to the north, as suggested by previous work in this region.

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Keywords Eastern Anti-Atla, Imiter granitoids, Pan-African, Saghro group, Sm-Nd isotopes
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Journal Journal of African Earth Sciences
Baidada, B. (Bouchra), Cousens, B, Alansari, A. (Abdelkhalek), Soulaimani, A. (Abderrahmane), Barbey, P. (Pierre), Ilmen, S. (Said), & Ikenne, M. (Moha). (2017). Geochemistry and Sm-Nd isotopic composition of the Imiter Pan-African granitoids (Saghro massif, eastern Anti-Atlas, Morocco): Geotectonic implications. Journal of African Earth Sciences. doi:10.1016/j.jafrearsci.2016.08.016