Petrogenesis of U- and Mo-bearing A2-type granite of the Gattar batholith in the Arabian Nubian Shield, Northeastern Desert, Egypt: Evidence for the favorability of host rocks for the origin of associated ore deposits-Reference-Cited by-同舟云学术

Petrogenesis of U- and Mo-bearing A2-type granite of the Gattar batholith in the Arabian Nubian Shield, Northeastern Desert, Egypt: Evidence for the favorability of host rocks for the origin of associated ore deposits

Published:2015-12 Issue: Volume:71 Page:57-81
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Mahdy Nasser M.^ORCID,El Kalioubi Baher A.,Wohlgemuth-Ueberwasser Cora C.^ORCID,Shalaby Mahmoud H.,El-Afandy Adel H.

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference134 articles.

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3. Modeling of REE fractionation in the acid melt fluoride–chloride fluid system;Abramov;Dokl. Earth Sci.,2001

4. Composition, age, and origin of the ~620Ma Humr Akarim and Humrat Mukbid A-type granites: no evidence for pre-Neoproterozoic basement in the Eastern Desert, Egypt;Ali;Int. J. Earth. Sci. (Geol. Rundsch.),2012

5. The Los Pedroches batholith (southern Spain): polyphase interplay between shear zones in transtension and setting of granites;Aranguren,1997

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