Origin of Cretaceous alkaline annular structures in the peri-cratonic terranes of the Reguibat Rise in Morocco: New constraints from carbonatite–silicate pairs and subsolidus processes-Reference-Cited by-同舟云学术

Origin of Cretaceous alkaline annular structures in the peri-cratonic terranes of the Reguibat Rise in Morocco: New constraints from carbonatite–silicate pairs and subsolidus processes

Published:2023-08 Issue: Volume:632 Page:121536
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Malainine Cheikh-Elwali,Ouabid Muhammad,Raji Otmane,Bodinier Jean-Louis,Parat Fleurice,El Messbahi Hicham,Dautria Jean-Marie,Jourani Es-Said,Khadiri Yazami Oussama,Garrido Carlos J.

Funder

Consejo Superior de Investigaciones Científicas

OCP Group

Université Mohammed VI Polytechnique

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference162 articles.

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5. Episodic alkaline igneous activity across Africa: Implications for the causes of continental break-up;Bailey,1992

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