P-T evolution of HP migmatitic paragneiss from the Beni Bousera metamorphic unit (internal Rif, Northern Morocco) constrained by phase equilibria modelling and melt reintegration-Reference-Cited by-同舟云学术

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P-T evolution of HP migmatitic paragneiss from the Beni Bousera metamorphic unit (internal Rif, Northern Morocco) constrained by phase equilibria modelling and melt reintegration

Published:2024-08-20 Issue: Volume: Page:1-25
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Essoualeh Oumaima¹,Aghzer Abdelmouhsine¹,Afiri Abdelkhaleq²,Abati Jacobo³,Mostadi Abdelfettah El¹,Benchekroun Fouad¹

Affiliation:

1. Department of Geology, Faculty of Sciences, University of Chouaib Doukkali, El Jadida, Morocco

2. Department of Geology, Faculty of Sciences and techniques, University of Moulay Smail, Errachidia, Morocco

3. Department of Mineralogy and Petrology, Faculty of Geological Sciences, University Complutense, Madrid, Spain

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2024.2392248

Reference112 articles.

1. Age of anatexis in the crustal footwall of the Ronda peridotites, S Spain

2. Refined Tectonic Evolution of the Betic‐Rif Orogen Through Integrated 3‐D Microstructural Analysis and Sm‐Nd Dating of Garnet Porphyroblasts

3. Afiri, A., Essaifi, A., Charroud, A., Aqnouy, M., Abdelrahman, K., Alali, A., and Abioui, M., 2023, Tectonometamorphic evolution of the migmatitic paragneisses of the filali unit, (Internal Rif, Morocco), Minerals, Vol. 13, p. 484.

4. Oligo-Miocene exhumation of the Beni-Bousera peridotite through a lithosphere-scale extensional shear zone

5. Crustal attenuation as a tracer for the emplacement of the Beni Bousera ultramafic massif (Betico-Rifean belt)

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