LES ROCHES MAGMATIQUES ET PYROCLASTIQUES DU CONGLOMERAT STRUNIEN DE L'OUED TIFLET (MESETA NORD OCCIDENTALE MAROCAINE): PETROGRAPHIE, GEOCHIMIE ET PROVENANCE

  • Hind El Haibi Laboratoire de Géologie Appliquée, Géomatique et Environnement, UH2C, Faculté des Sciences Ben M'sik Casablanca, Maroc
  • Hassan El Hadi Laboratoire de Géologie Appliquée, Géomatique et Environnement, UH2C, Faculté des Sciences Ben M'sik Casablanca, Maroc
  • Abdelfatah Tahiri Laboratoire de Géologie et de Télédétection, URAC-46 Université Mohammed V de Rabat, Institut Scientifique, Rabat, Maroc
  • Ibtissam Bensalah Office National des Hydrocarbures et des Mines (ONHYM), Maroc
  • Ayoub El Maidani Office National des Hydrocarbures et des Mines (ONHYM), Maroc

Abstract

In the north boundary of the Sidi Bettache basin (northwestern morrocan Meseta), the strunian period is characterized by coarse detrital sedimentation, among them the limestone conglomerate of Tiflet river. This conglomerate is rich in magmatic pebbles varying by nature and shape. Petrographical and geochemical studies allow distinguishing eleven facies, which generally correspond to basic, including gabbros, intermediate or acids rocks. Tuffs, sulfides bearing-rocks and oxides are also identified. Age of this magmatic rocks is discussed.

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Published
2015-05-29
How to Cite
El Haibi, H., El Hadi, H., Tahiri, A., Bensalah, I., & El Maidani, A. (2015). LES ROCHES MAGMATIQUES ET PYROCLASTIQUES DU CONGLOMERAT STRUNIEN DE L’OUED TIFLET (MESETA NORD OCCIDENTALE MAROCAINE): PETROGRAPHIE, GEOCHIMIE ET PROVENANCE. European Scientific Journal, ESJ, 11(15). Retrieved from https://eujournal.org/index.php/esj/article/view/5622
Issue
Vol 11 No 15 (2015): ESJ May Edition
Section
Articles