This work is based on the compilation and re-evaluation of the most significant data, either
personal or from the literature, concerning the Moroccan Variscides. The latter constitute the …

This paper attempts to describe the Neoproterozoic–Cambrian lithostratigraphic
successions occurring on the West African craton and in the surrounding Pan-African fold …

In Northern Africa deformed Paleozic rocks are observed, mainly in Morocco where they are
present in two structural domains:(i) the southern domain, ie the Anti-Atlas belt. In this …

We present a δ13C record from the Anti-Atlas mountains of Morocco and place it in the
context of a detailed regional tectonostratigraphy. We place the litho-and chemostratigraphic …

U–Pb–Hf of detrital zircons from diverse Cambrian units in Morocco and Sardinia were
investigated in order to clarify the sandstone provenance and how it evolved with time, to …

Abstract The post-Pan-African evolution of the northern border of the West African Craton is
largely controlled by the remobilisation of Late Neoproterozoic basement faults. The Upper …

Large igneous provinces and associated silicic magmatism can have a significant global
climatic effect, so we explored the relationship between the large igneous province record …

The world-class Imiter silver deposit, in the Anti-Atlas Mountains of Morocco, is a
Neoproterozoic epithermal vein deposit genetically associated with a felsic volcanic event …

Dans l'Anti-Atlas (sud du Maroc), la couverture du Néo-protérozoïque supérieur, discordante
sur les structures panafricaines, s' organise en «séries» volcaniques et détritiques (Groupe …

In the northwestern border of the West African craton (North Gondwana), a transition from
late Neoproterozoic subduction/collision to Cambrian rift processes was recorded in the Anti …