Origin of the post-orogenic dyke swarms of Saharan Metacraton, at Qaret El-Maiyit-Bir Safsaf area, southwest Egypt: Constraints on the magmatic–tectonic processes at the end of the Precambrian-Reference-Cited by-同舟云学术

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Origin of the post-orogenic dyke swarms of Saharan Metacraton, at Qaret El-Maiyit-Bir Safsaf area, southwest Egypt: Constraints on the magmatic–tectonic processes at the end of the Precambrian

Published:2024-11 Issue: Volume:219 Page:105378
ISSN:1464-343X
Container-title:Journal of African Earth Sciences
language:en
Short-container-title:Journal of African Earth Sciences

Author:

Mashaal Shaaban,Abdel-Bary Amany,Ragab Azza

Publisher

Elsevier BV

Reference138 articles.

1. Geochemistry and Petrogenesis of Dike Rocks of Wadi Rimthi Area, South Central Sinai, Egypt;Abdel-Bary,2014

2. Petrology and geochemistry of late Precamberian old dykes swarms in Southwestern Sinai;Abdel-Karim;Egypt Acta. Min. Petrogr. Szeged, Hungary,1993

3. The saharan metacraton;Abdelsalam;J. Afr. Earth Sci.,2002

4. Upper mantle structure of the saharan metacraton;Abdelsalam;J. Afr. Earth Sci.,2011

5. Petrogenesis and tectonic implications of Tonian island arc volcanic rocks from the Gabgaba Terrane in the Arabian-Nubian Shield (NE Sudan);Adam;J. Asian Earth Sci.,2022

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