Pouclet, A., Ouazzani, H. and Fekkak, A. (2008) The Cambrian Volcano-Sedimentary Formations of the Westernmost High Atlas (Morocco): Their Place in the Geodynamic Evolution of the West African Palaeo-Gondwana Northern Margin. Geological Society, London, Special Publications, 297, 303-327.
http://dx.doi.org/10.1144/SP297.15

has been cited by the following article:

• TITLE: The Late Neoproterozoïc Continental Tholeiitic Basalts of the Toubkal Inlier (Western High-Atlas, Morocco): A Post-Pan-African Rifting Witness in the Northern Margin of the West African Craton

  AUTHORS: Ghalem Zahour, Hassan El Hadi, Abdelfatah Tahiri, Youssef Zerhouni, Saida Alikouss, Rachid Zahour, Aicha Reddad

  KEYWORDS: Toubkal Inlier, Late Neoproterozoïc, Continental Tholeiites, Rift, West African Craton

  JOURNAL NAME: Open Journal of Ecology, Vol.6 No.8, July 21, 2016

  ABSTRACT: The late Neoproterozoïc Toubkal inlier (Ancient Massif of the High-Atlas, Morocco) contains two igneous basaltic series (Tircht and Sidi Chamharouch). Investigated rocks display characteristics of within-plate continental tholeiitic and are similar to rocks originated in orogenic contexts. The geochemical results allow the assumption that subduction active processes are indirectly responsible for the genesis of theses rocks. The orogenic signature is linked probably to a Pan-African magmatic source previously metasomatized in the northern margin of the West African Craton.