The Jbel Saghro is interpreted as part of a long-lived silicic large igneous province. The area
comprises two lithostructural complexes. The Lower Complex consists of folded …

Abstract In the Moroccan Eastern Anti-Atlas, the Thaghassa intrusion-related gold deposit is
hosted in hornfelsed metasedimentary rocks that lie adjacent to the Ikniwn granodiorite …

We explore the connections between crustal shortening, volcanism, and mantle dynamics in
the Atlas of Morocco. In response to compressional forces and strain localization, this …

Tectonic and micro-tectonic studies at different scales are of primary importance in a modern
metallogenic investigation. In the Ougnat massif of the eastern Anti-Atlas belt (Morocco), the …

This study provides interpreted aeromagnetic databases combined with structural and
metallographic investigation to examine the surface versus subsurface faults interaction and …

At the northern border of the West African Craton (WAC), the Saghro massif of the Moroccan
Anti-Atlas belt is renowned for its tectonic complexity inherited from Pan-African, Variscan …

Salt tectonics play a critical role on passive margins evolution controlling aspects like
structural style, subsidence patterns and thermal history, amongst others. The salt-bearing …

New lithostratigraphical and structural data provide a better assessment of the still
controversial metallogenetic context of the world-class Ag–Hg Imiter deposit, located in the …

Abstract The High Atlas belt of Morocco is a doubly vergent intracontinental belt formed
during Cenozoic convergence between the African and Eurasian plates. This belt is …

Abstract From the Neoproterozoic to Cenozoic, different extensional and transpressional
tectonics events occurred during the Pan-African, Variscan and Alpine orogenic cycles in the …