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<title lang=en>The southern and central parts of the “Souttoufide” belt, Northwest Africa</title>
<creator>Villeneuve, M.</creator>
<creator>Gärtner, A.</creator>
<creator>Youbi, N.</creator>
<creator>El Archi, A.</creator>
<creator>Vernhet, E.</creator>
<creator>Rjimati, Ech-Cherki</creator>
<creator>Linnemann, Ulf</creator>
<creator>Bellon, H.</creator>
<creator>Gerdes, A.</creator>
<creator>Guillou, O.</creator>
<creator>Corsini, M.</creator>
<creator>Paquette, J.-Louis</creator>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Senckenberg Naturhistorische Sammlungen Dresden ; Museum für Mineralogie und Geologie</contributor>
<contributor>Faculty of Sciences Semlalia ; University Cadi Ayyad (UCA)</contributor>
<contributor>Département de Géologie ; Université Chouaib Doukkali</contributor>
<contributor>Université des Antilles et de la Guyane (UAG)</contributor>
<contributor>Service géologique du Maroc</contributor>
<contributor>UMR CNRS 2761 - Université de Bretagne occidentale</contributor>
<contributor>Institut für Geowissenschaften, Goethe-Universität, Frankfurt am Main</contributor>
<contributor>Géoazur (GEOAZUR) ; Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire Magmas et Volcans (LMV) ; Université Blaise Pascal - Clermont-Ferrand 2 (UBP) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Jean Monnet [Saint-Étienne] (UJM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0899-5362</source>
<source>Journal of African Earth Sciences</source>
<publisher>Elsevier</publisher>
<identifier>hal-01382815</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01382815</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01382815</source>
<source>Journal of African Earth Sciences, Elsevier, 2015, 112 (B), pp.451 - 470. 〈10.1016/j.jafrearsci.2015.04.016〉</source>
<identifier>DOI : 10.1016/j.jafrearsci.2015.04.016</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jafrearsci.2015.04.016</relation>
<language>en</language>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The Souttoufide belt is situated between the High-Atlas in the north, the Mauritanides in the south and the West African Craton as well as the Tindouf basin in the east. Thus, this belt is a part of the West African fold belt system which surrounds the West African Craton. Outcrops occur only in three areas, while the rest of the Souttoufide belt is covered by Meso- to Cenozoic sediments. These areas are, from the south to the north, the Adrar Souttouf Massif, the Smara Zemmour area, and the western part of the Anti-Atlas. Because of the continuing processing and numerous publications, the Anti-Atlas cannot be dealt with in detail. Fundamental geological work in both of the other areas was mainly done during the second third of the 20th century, followed by several decades of inactivity. Numerous studies were done in the Adrar Souttouf massif during the last decade, while the Smara-Zemmour area still remains poorly investigated. Most of them were focused on geochronological analyses and geochemistry. Accordingly, the obtained data led to a new interpretation. The Adrar Souttouf is interpreted as a Pan-African belt exhibiting a Neoproterozoic island arc reworked by the Variscan collision between the North American Craton (NAC) and the West African Craton (WAC). The Smara-Zemmour area is considered as the external part of this Variscan belt thrusted onto the Palaeozoic Tindouf basin. The western Anti-Atlas as considered as a Pan-African active margin reworked during the Variscan orogen. Together, these three areas, lead to the hypothesis of a Late Pan-African belt capped by the Early and Middle Palaeozoic covers and then affected by the Middle Carboniferous tectonic event (330 Ma) related to the Pangaean assembly. Correlations with adjacent belts (Mauritanides and Anti-Atlas) are considered.</description>
<date>2015-05-09</date>
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