The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt (Morocco): Evidence for Polyphase Rifting and Related Magmatic Activity-Reference-Cited by-同舟云学术

The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt (Morocco): Evidence for Polyphase Rifting and Related Magmatic Activity

Published:2019-08 Issue:8 Volume:38 Page:2894-2918
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Gimeno‐Vives Oriol¹^ORCID,Mohn Geoffroy¹^ORCID,Bosse Valérie²,Haissen Faouziya³,Zaghloul Mohamed Najib⁴,Atouabat Achraf⁴,Frizon de Lamotte Dominique¹^ORCID

Affiliation:

1. Département Géosciences et Environnement (GEC) Université de Cergy‐Pontoise Cergy‐Pontoise France

2. Laboratoire Magmas et Volcans (UMR 6524), CNRS Université Blaise Pascal Clermont‐Ferrand France

3. Faculté des Sciences Ben M'sik, Département de Géologie Université Hassan II de Casablanca Casablanca Morocco

4. Department of Earth Sciences, Faculty of Sciences and Techniques University Abdelmalek Essaadi Tangiers Morocco

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019TC005508

Reference111 articles.

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3. Tholeitic basalts and ophiolitic complexes of the Mesorif Zone (External Rif, Morocco) at the Jurassic‐Cretaceous boundary and the importance of the Ouerrha Accident in the palaeogeographic and geodynamic evolution of the Rif Mountains;Benzaggagh M.;Boletín geológico y minero,2016

4. Oceanic units in the core of the External Rif (Morocco): Intramargin hiatus or South-Tethyan remnants?

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