Late Neoproterozoic banded iron formation (BIF) in the central Eastern Desert of Egypt: Mineralogical and geochemical implications for the origin of the Gebel El Hadid iron ore deposit-Reference-Cited by-同舟云学术

Late Neoproterozoic banded iron formation (BIF) in the central Eastern Desert of Egypt: Mineralogical and geochemical implications for the origin of the Gebel El Hadid iron ore deposit

Published:2015-09 Issue: Volume:69 Page:380-399
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Khalil Khalil I.,El-Shazly Aley E.,Lehmann Bernd

Funder

NSF OISE

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference111 articles.

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3. Geology of the basement rocks in the eastern half of the belt between Latitudes 25° 30′ and 26° 30′ N Central Eastern Desert, Egypt;Akaad;Geol. Surv. Egypt,2002

4. Geochemistry, Nd isotopes and U–Pb SHRIMP zircon dating of Neoproterozoic volcanic rocks from the Central Eastern Desert of Egypt: new insights into the ~750Ma crust-forming event;Ali;Precambrian Res.,2009

5. Geochemical U–Pb zircon and Nd isotope investigations of the Neoproterozoic Ghawjah Metavolcanic rocks, Northwestern Saudi Arabia;Ali;Lithos,2010

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