Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Ech Cherki Rjimati"'
Autor:
Abdelkader Mokhtari, Philippe Rossi, Omar Saddiqi, Philippe Lach, Ech Cherki Rjimati, Ahmed Chalouan, André Michard
Publikováno v:
Comptes Rendus Geoscience. 350:299-309
This work concerns the northernmost limit of the West African Craton (WAC) and Variscan WAC-related terranes of NW Africa. Based on newly obtained radiometric age of an oceanic gabbro from the “Mesorif Suture Zone” of the External Rif Belt, we pr
Autor:
Lahsen Aït Brahim, Lahssen Baidder, Abderrahmane Soulaimani, André Michard, Youssef Raddi, Omar Saddiqi, Hassan Ouanaimi, Ech-Cherki Rjimati
Publikováno v:
Comptes Rendus Geoscience. 349:81-90
The Saghro Group (SG) is a folded, low-grade volcano-sedimentary series up to 8 km thick that crops out within and to the north of the Pan-African suture zone in the central and eastern Anti-Atlas. Here we describe the SG of the Ougnat inliers that a
Autor:
A. Eddebbi, Abderrahmane Soulaimani, Youssef Raddi, Ech-Cherki Rjimati, André Michard, Lahssen Baidder, A. Fekkak
Publikováno v:
Journal of African Earth Sciences. 119:204-225
Conflicting views are expressed in literature concerning fold interference patterns in thick-skinned tectonic context (e.g. Central Anti-Atlas and Rocky Mountains-Colorado areas). Such patterns are referred to superimposed events with distinct orient
Autor:
Lahssen Baidder, André Michard, Ech-Cherki Rjimati, Omar Saddiqi, Youssef Raddi, H. Ouanaimi, Abderrahmane Soulaimani
Publikováno v:
Journal of African Earth Sciences. 98:94-112
The post-Pan-African evolution of the northern border of the West African Craton is largely controlled by the remobilisation of Late Neoproterozoic basement faults. The Upper Ediacaran volcanic and volcano-sedimentary sequences of the Ouarzazate Grou
Autor:
Ech-Cherki Rjimati, Mohamed Benzaggagh, Abdelkader Mokhtari, Philippe Rossi, André Michard, Ahmed Chalouan, Omar Saddiqi, Abdelkhader El Maz
Publikováno v:
Journal of Geodynamics
Journal of Geodynamics, Elsevier, 2014, 77, pp.4-21. ⟨10.1016/j.jog.2013.10.003⟩
Journal of Geodynamics, Elsevier, 2014, 77, pp.4-21. ⟨10.1016/j.jog.2013.10.003⟩
International audience; he aim of this paper is to describe the mafic rocks that crop out in the central-western Mesorif Zone (External Rif Belt), and discuss their geodynamic signification. Basalt flows, olistoliths and breccias occur in Oxfordian-B
Autor:
Kevin Hefferan, Pilar Montero, Omar Saddiqi, José F. Molina, Fernando Bea, Abderrahmane Soulaimani, H. Ouanaimi, Michel Corsini, A. Michard, Ech-Cherki Rjimati
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2019, 157, pp.103501. ⟨10.1016/j.jafrearsci.2019.05.009⟩
Journal of African Earth Sciences, Elsevier, 2019, 157, pp.103501. ⟨10.1016/j.jafrearsci.2019.05.009⟩
International audience; South of the Pan-African suture zone of the Anti-Atlas, the Agadir Melloul inlier exhibits several crests of nearly vertical conglomeratic quartzite beds inserted in Paleoproterozoic granites. These enigmatic rocky walls have
Autor:
Omar Saddiqi, Ech-Cherki Rjimati, Abderrahmane Soulaimani, Lahssen Baidder, Christian Hoepffner, André Michard, Hassan Ouanaimi
Publikováno v:
Tectonophysics. 492:1-24
This work is based on the compilation and re-evaluation of the most significant data, either personal or from the literature, concerning the Moroccan Variscides. The latter constitute the only, moderately disturbed or even undisturbed part of the Sou
Autor:
Elodie Vernhet, Abdelkrim El Archi, Jean-Louis Paquette, Hervé Bellon, Andreas Gärtner, Michel Corsini, Michel Villeneuve, Omar Guillou, Ech-Cherki Rjimati, Ulf Linnemann, Axel Gerdes, Nasrrddine Youbi
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2015, 112 (B), pp.451-470. ⟨10.1016/j.jafrearsci.2015.04.016⟩
Journal of African Earth Sciences, 2015, 112 (B), pp.451-470. ⟨10.1016/j.jafrearsci.2015.04.016⟩
Journal of African Earth Sciences, Elsevier, 2015, 112 (B), pp.451-470. ⟨10.1016/j.jafrearsci.2015.04.016⟩
Journal of African Earth Sciences, 2015, 112 (B), pp.451-470. ⟨10.1016/j.jafrearsci.2015.04.016⟩
International audience; 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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ae9aa0bf3369266143a1a5afbf4193e
https://hal.archives-ouvertes.fr/hal-01382815
https://hal.archives-ouvertes.fr/hal-01382815
Publikováno v:
Geoheritage, Geoparks and Geotourism ISBN: 9783319107073
The remote regions of Southern Morocco are rich in outstanding geological landscapes and outcrops not well known to the general public. In this paper, we propose two east-trending geotrails (transverse to the regional trend of the structures) with a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f371bc1fe86bab6e590b6ab8c80cb01d
https://doi.org/10.1007/978-3-319-10708-0_6
https://doi.org/10.1007/978-3-319-10708-0_6
Autor:
Ech-Cherki Rjimati, Omar Saddiqi, Philippe Rossi, Ahmed Chalouan, Abdelkader Mokhtari, André Michard
Publikováno v:
Bulletin de la Société Géologique de France
Bulletin de la Société Géologique de France, Société géologique de France, 2014, 185 (5), ⟨10.2113/gssgfbull.185.5.313⟩
Bulletin de la Société Géologique de France, Société géologique de France, 2014, 185 (5), ⟨10.2113/gssgfbull.185.5.313⟩
Ophiolite slivers have been described recently in the core of the External zones of the Central Rif belt. The present work aims at illustrating new ophiolite slivers further east and discussing the structural position and tectonic emplacement of all
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f46224f6c65e2b46830d373725821529
https://hal-brgm.archives-ouvertes.fr/hal-01318446
https://hal-brgm.archives-ouvertes.fr/hal-01318446