Arid
Geochemistry, mineralogy, and radioactivity of the Abu Furad Area, Central Eastern Desert, Egypt
El Mezayen A M; Abu Zeid E K; Hosny W S; El-Feky M G; Omar S M; Taalab S A
来源期刊Acta Geochimica
ISSN2096-0956
出版年2019
卷号38期号:2页码:307-326
英文摘要Abu Furad is in the Central Eastern Desert, Egypt. It comprises metasediments, metavolcanics, metagabbros, syn- to late-orogenic granites, and post-orogenic granites, in addition to numerous dykes and veins of different shapes and composition invading all the older rocks cropping out in the study area. Field, petrographic, mineralogical, and chemical investigations led to the classification of Abu Furad granites as quartz diorite, tonalite, granodiorite, and syenogranites.Major oxide and trace element data revealed that the syn- to late-orogenic granites and post-orogenic granites are peraluminous. Syn- to lateorogenic granites originated from calc-alkaline volcanic arc-related magma; while the post-orogenic granites (syenogranite) are highly fractionated, calc-alkaline granite from a within plate regime. Radiometrically, the studied quartz diorite, tonalite, and granodiorite had lower uranium and thorium contents and higher eU/eTh ratios than the syenogranites. This may indicate that the syn- to lateorogenic rocks originated from sources depleted in these elements. The average eTh/eU ratio of syenogranites was higher than that of average continental crust, suggesting that the syenogranites are relatively depleted in U. The studied altered syenogranites were strongly enriched in U and Th compared to the Earths crust. On the other hand, the average of eU in pegmatites is lower than the global average for uraniferous pegmatites. The most recorded accessory minerals in the altered syenogranites were thorite, fergusonite, samarskite, columbite, zircon, monazite, xenotime, apatite, fluorite, sphene, atacamite, and malachite, in addition to chromium and nickel inclusions.
英文关键词Hydrothermal alterations Major oxide and trace elements Radiometry Mineralogy Geochemistry Altered syenogranites Egypt
类型Article
语种英语
收录类别CSCD
WOS研究方向Geology
CSCD记录号CSCD:6471552
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/336091
作者单位El Mezayen A M, Geology Department, Faculty of Science, Al Azhar University, Cairo, Egypt.; Taalab S A, Geology Department, Faculty of Science, Al Azhar University, Cairo, Egypt.; Abu Zeid E K, Nuclear Material Authority, Cairo, Egypt.; Hosny W S, Nuclear Material Authority, Cairo, Egypt.; El-Feky M G, Nuclear Material Authority, Cairo, Egypt.; Omar S M, Nuclear Material Authority, Cairo, Egypt.
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El Mezayen A M,Abu Zeid E K,Hosny W S,et al. Geochemistry, mineralogy, and radioactivity of the Abu Furad Area, Central Eastern Desert, Egypt[J],2019,38(2):307-326.
APA El Mezayen A M,Abu Zeid E K,Hosny W S,El-Feky M G,Omar S M,&Taalab S A.(2019).Geochemistry, mineralogy, and radioactivity of the Abu Furad Area, Central Eastern Desert, Egypt.Acta Geochimica,38(2),307-326.
MLA El Mezayen A M,et al."Geochemistry, mineralogy, and radioactivity of the Abu Furad Area, Central Eastern Desert, Egypt".Acta Geochimica 38.2(2019):307-326.
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