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Geological Society, London, Special Publications; 2008; v. 297; p. 433-452;
DOI: 10.1144/SP297.20
© 2008 Geological Society of London

The Variscan orogeny along the West African craton

The Anti-Atlas chain (Morocco): the southern margin of the Variscan belt along the edge of the West African craton

Abderrahmane Soulaimani1,2 & Martin Burkhard3,4

1 Université Cadi Ayyad, Faculté des Sciences Semlalia, av. Moulay Abdellah, BP 2390, Marrakech, Morocco
2 Present address: 18 rue Stephenson, 59000 Lille, France (e-mail: soulaimani{at}ucam.ac.ma)
3 Institut de Géologie, Université de Neuchâtel, rue Émile-Argand 11, CP 2, 2007 Neuchâtel, Switzerland
4 Deceased August 2006

Broadly synchronous circum-Atlantic Variscan–Alleghanian orogenic belts developed during the Late Palaeozoic Gondwana–Laurentia collision. In the northern part of the West African craton (WAC), the Variscan orogeny produced basement-controlled structures in the Anti-Atlas, which represents the pericratonic foreland, now located south of the Variscan domains of Morocco and north of the Mauritanides belt. New structural field observations document the strong involvement of the basement and the inversion and folding of the Palaeozoic sedimentary basins at the edge the WAC. Two contrasting domains differently responding to regional NW–SE shortening are recognized: (1) a narrow belt along the Atlantic coast characterized by thin-skinned folding and ESE-vergent thrusting (para-autochthonous Anti-Atlas); (2) a large area between the WAC sensu stricto and the South Atlas front showing huge basement uplifts amidst a folded Palaeozoic cover with upright polyharmonic folds (autochthonous Anti-Atlas). The structural trend of the basement inliers is inherited at least in some case from previous Proterozoic fractures. Compressional reactivations led to basement uplift and concomitant folding of the Palaeozoic cover. Cover series are horizontally shortened by mostly upright symmetrical buckle folds of various wavelengths in response to thickness variations between abundant incompetent silt and shale horizons and rare competent carbonate and quartzite beds. Deformation is greatest near the borders of and between closely spaced basement uplifts. Regionally, deformation intensity decreases, either abruptly or progressively, towards the SE and it vanishes within the undeformed Tindouf basin.