Origin and geotectonic evolution of Mir Tertiary basaltic andesite dykes, Western Desert, Egypt: Constraints from mineral and bulk-rock chemistry-Reference-Cited by-同舟云学术

Origin and geotectonic evolution of Mir Tertiary basaltic andesite dykes, Western Desert, Egypt: Constraints from mineral and bulk-rock chemistry

Published:2018-08-10 Issue:4 Volume:54 Page:2274-2287
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Farahat Esam S.¹,Ali Shehata¹^ORCID

Affiliation:

1. Geology Department, Faculty of Science; Minia University; Minya Egypt

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/gj.3296/fullpdf

Reference91 articles.

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3. Major element composition, mama type and tectonic environment of Mesozoic to Recent basalts, Egypt: A review;Abdel Monem;Bulletin of the Faculty of Science, K.A.U, Jeddah,1981

4. Late Proterozoic Pan African tectonic evolution of the Egyptian part of the Arabian-Nubian Shield;Abdel-Meguid;MERC Ain Shams University Earth Science Series,1992

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