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Stratigraphic and tectonic architecture of the Middle Jurassic-Upper Cretaceous at the southern front of the Central High Atlas (Morocco): a cartographic revision

Author

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  • M. Benvenuti
  • C. Cavallina
  • G. Moratti
  • M. Papini

Abstract

The Middle Jurassic (Bathonian)-Upper Cretaceous (Maastrichtian) deposits exposed at the southern front of the Central High Atlas (CHA, Southern Morocco) include thick fluvial successions largely undifferentiated in previous studies. These continental strata record a long period of relief formation due to crustal shortening and subsequent denudation that predated the Cenozoic, syn-collisional, tectonic inversion of the CHA. This study, carried out through mapping along more than 270 km between Ouarzazate and Errachidia towns, firstly proposes a rock-stratigraphic unified scheme based on a framework of unconformity-bounded stratigraphic units, including sub-units, differentiated for their specific depositional meaning. Secondly, the geological maps and related cross-sections illustrate the evidence of syn-depositional shortening with distinct deformation styles, outlining pre- and syn-collisional tectonic inversion.

Suggested Citation

  • M. Benvenuti & C. Cavallina & G. Moratti & M. Papini, 2022. "Stratigraphic and tectonic architecture of the Middle Jurassic-Upper Cretaceous at the southern front of the Central High Atlas (Morocco): a cartographic revision," Journal of Maps, Taylor & Francis Journals, vol. 18(2), pages 530-539, December.
  • Handle: RePEc:taf:tjomxx:v:18:y:2022:i:2:p:530-539
    DOI: 10.1080/17445647.2022.2101950
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