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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Altered granitic rocks, Nusab El Balgum Area, Southwestern Desert, Egypt: Mineralogical and geochemical aspects of REEs
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Altered granitic rocks, Nusab El Balgum Area, Southwestern Desert, Egypt: Mineralogical and geochemical aspects of REEs

机译:埃及西南沙漠努萨布·巴尔古姆地区花岗岩岩蚀变:稀土元素的矿物学和地球化学方面

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摘要

Gabel Nusab El Balgum is located in the northern part of Bir Safsaf Area Southwestern Desert, Egypt (about 600 km southwest of Aswan City) and covers an area of about 40 km(2). A few workers have investigated the Nusab El Balgum Area from the mineralogical and geochemical point of view. The area consists mainly of Devonian sandstone, Permo-Triassic volcanic rocks, altered granitic rocks and post-granitic dykes. The altered granitic rocks (silicified and kaolinized) have undergone several hydrothermal alteration processes and were subjected to different types of alteration (hematitization, carbonatization, kaolinization, sericitization and silicification) and are characterized by extreme enrichment in rare metals (such as Zr, Nb, Y and REEs).
机译:Gabel Nusab El Balgum位于埃及比尔萨夫萨夫地区西南沙漠的北部(阿斯旺市西南约600公里),面积约40公里(2)。一些工人从矿物学和地球化学的角度研究了努萨布·巴尔干地区。该地区主要由泥盆纪砂岩,二叠系-三叠纪火山岩,蚀变花岗质岩和后砾岩脉组成。蚀变的花岗岩(硅化和高岭土)经历了几次热液蚀变过程,并经历了不同类型的蚀变(赤铁矿化,碳化,高岭土化,硅化和硅化),其特征是稀有金属(如Zr,Nb, Y和REE)。

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