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The External Domain of Maghrebides Belt on the North–East of Algeria, Souk Ahras Segment: Definition of Structural Units, Block Structure and Timing of Thrusts Setting

  • Abdallah ChabbiEmail author
  • Asma Chermiti
  • Abdelmadjid Chouabbi
  • Mohamed Benyoussef
Conference paper
Part of the Advances in Science, Technology & Innovation book series (ASTI)

Abstract

The detailed geological mapping supported by micropaleontological, tectonic and structural data of Souk Ahras region (North–East of Algeria) made it possible to define the main structural units of the external domain of the Maghrebides belt in the North–East of Algeria. The study area shows a block structure illustrating an allochthonous domain (Numidian unit, the northern Tellian unit and the southern Tellian) thrusting a folded para-autochthonous domain (the scaly unit of the Sellaoua type and the Dj. Graout unit). The current structure is edified into three phases at least: post Langhian phase, Tortonian phase and Pliocene phase.

Keywords

External domain Allochthonous domain Tellian nappes Sellaoua unit Souk Ahras Algeria 

References

  1. 1.
    Bouillin, J.-P.: Le bassin maghrébin: une ancienne limite entre l’Europe et l’Afrique à l’Ouest des Alpes. Bull. Soc. geol. France 8(4), 547–558 (1986)CrossRefGoogle Scholar
  2. 2.
    Roure, F., Casero, P., Addoum, B.: Alpine inversion of the North African margin and delamination of its continental lithosphere. Tectonics 31, TC3006 (2012).  https://doi.org/10.1029/2011tc002989CrossRefGoogle Scholar
  3. 3.
    Vila, J.M.: La chaine alpine d’Algérie orientale et des confins Algéro-Tunisien. Phd thesis, Univ. Pierre et Marie Curie (Paris VI), France, 665p (1980)Google Scholar
  4. 4.
    David, L.: Etude géologique de la haute Medjerda. Bulletin du Service de la carte géologique de l’Algérie, n° 11, Algérie, 304p (1956)Google Scholar
  5. 5.
    Rouvier, H.: Géologie de l’extrême Nord tunisien : tectoniques et paléogéographies superposées à l’extrémité orientale de la chaîne nord-maghrébine. Phd thesis, P et M. C. university, Paris, France, 898p (1977)Google Scholar
  6. 6.
    Vila, J.M., Feinberg, H., Lahondère, J.C., Gourinard, Y., Chouabbi, A., Magné, J., Durand-Delga, M.: The sandy uppermost Oligocene channel and the Miocene of Sidi- Affif area in their East Algerian structural setting -the Saharan Origin of the Numidian and the calendar of the Miocene overthrusts. Comptes Rendus De l’Academie Des Sciences Serie 2 320(10), 1001–1009 (1995)Google Scholar
  7. 7.
    Riahi, S., Soussi, M., Boukhalfa, K., Ben Ismail Lattrache, K., Dorrik, S., Khomsi, S., Bedir, M.: Stratigraphy, sedimentology and structure of the Numidian Flysch thrust belt in northern Tunisia. J. Afr. Earth Sci. 57, 109–126 (2010)CrossRefGoogle Scholar
  8. 8.
    Chabbi, A., Chouabbi, A., Chermiti, A., Ben Youssef, M., Kouadria, T., Ghanmi, M.: La mise en évidence d’une nappe de charriage en structure imbriquée: Cas de la nappe tellienne d’Ouled Driss, Souk-Ahras, Algérie. Courrier du Savoir, Algeria. N°21, pp. 149–156 (2016)Google Scholar
  9. 9.
    Bracene, R., Frizon de Lamotte, D.: The origin of intraplate deformation in the Atlas system of western and central Algeria: from Jurassic rifting to Cenozoic-Quaternary inversion. Tectonophysics 357, 207–226 (2002)CrossRefGoogle Scholar

Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  • Abdallah Chabbi
    • 1
    • 2
    Email author
  • Asma Chermiti
    • 3
  • Abdelmadjid Chouabbi
    • 2
  • Mohamed Benyoussef
    • 3
  1. 1.Mohamed Cherif Messaadia UniversitySouk AhrasAlgeria
  2. 2.Geodynamics and Natural Resources LaboratoryBadji Mokhtar universitySidi Amar, AnnabaAlgeria
  3. 3.Water Researches and Technologies Center, Ecopark of Borj CedriaSolimanTunisia

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