The intracontinental High Atlas belt: geological overview and pending questions

The High Atlas intracontinental belt is an inverted rift formed along the Northwest African Craton, between the Central Atlantic Ocean and the Africa-Eurasia plates’ boundaries. Due to its particular location at this triple junction, the Moroccan High Atlas is a good example to investigate the tecto...

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Veröffentlicht in:	Arabian journal of geosciences 2021-06, Vol.14 (12), Article 1071
Hauptverfasser:	Skikra, Hamza, Amrouch, Khalid, Soulaimani, Abderrahmane, Leprêtre, Rémi, Ouabid, Muhammad, Bodinier, Jean-Louis
Format:	Artikel
Sprache:	eng
Schlagworte:	Anticlines Asthenosphere Basements Belts Carbonates Cenozoic Compacting Complexity Cratons Cretaceous Crustal shortening Deformation Drowning Earth and Environmental Science Earth science Earth Sciences Eocene Evaporites Fault lines Faults Geological faults Jurassic Lithosphere Magma Neogene Oceanic crust Orogeny Orography Platforms (geology) Questions Review Paper Ridges Rifting Salts Sciences of the Universe Seafloor spreading Tectonics Triassic Uplift
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