Using Portable Gamma‐Ray Spectrometry for Testing Uranium Migration: A Case Study from the Wadi El Kareim Alkaline Volcanics, Central Eastern Desert, Egypt.

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Title: Using Portable Gamma‐Ray Spectrometry for Testing Uranium Migration: A Case Study from the Wadi El Kareim Alkaline Volcanics, Central Eastern Desert, Egypt.
Authors: DESSOUKY, Osama K.1, ALI, Hani H.1
Source: Acta Geologica Sinica (English Edition). Dec2018, Vol. 92 Issue 6, p2214-2232. 19p.
Subject Terms: *Migration of uranium, *Gamma ray spectrometry, *Radioactivity, *Geochemistry, *Volcanism, *Geology
Geographic Terms: Egypt
Abstract: The 300±20 Ma anomalously radioactive trachytes of Wadi El Kareim, central Eastern Desert, are a significant example of U‐mineralization related to the alkaline volcanics in Egypt. Extensive portable gamma‐ray spectrometric data has been utilized to identify geological factors controlling uranium mobility in the geological units along the three detailed study locations of Kab Al‐Abyad, South Wadi (W) Al‐Tarafawy and W. Al‐Farkhah; their eTh/eU ratios averaging around 4.1, 3.7 and 5.6 respectively. Quantitative analysis with the integration of mobility maps and geological studies suggest two systems controlling U‐migration within the geological units (confined system and unconfined system). In the confined system, the syngenetically formed U have experienced mobility after leaching and are redistributed in the presence of an incorporation carrier during transportation (probably as carbonate complexes). Then the retardant for uranium is achieved by sorption or by coprecipitation with the aid of Fe oxy‐hydroxide, and finally the formation of immobile secondary U‐bearing minerals takes place along a lithogeochemical trap. In contrast to the confined system, the unconfined one is basically lacking the lithogeochemical trap which influences the final accumulation of U‐bearing minerals. The radioactivity of the trachyte rocks arises from the radioactive minerals uranophane and beta‐uranophane with U‐ and/or Th‐bearing minerals samarskite, Th‐rich REE silicates, monazite and allanite. [ABSTRACT FROM AUTHOR]
Database: Energy & Power Source
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  Data: <searchLink fieldCode="JN" term="%22Acta+Geologica+Sinica+%28English+Edition%29%22">Acta Geologica Sinica (English Edition)</searchLink>. Dec2018, Vol. 92 Issue 6, p2214-2232. 19p.
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  Data: *<searchLink fieldCode="DE" term="%22Migration+of+uranium%22">Migration of uranium</searchLink><br />*<searchLink fieldCode="DE" term="%22Gamma+ray+spectrometry%22">Gamma ray spectrometry</searchLink><br />*<searchLink fieldCode="DE" term="%22Radioactivity%22">Radioactivity</searchLink><br />*<searchLink fieldCode="DE" term="%22Geochemistry%22">Geochemistry</searchLink><br />*<searchLink fieldCode="DE" term="%22Volcanism%22">Volcanism</searchLink><br />*<searchLink fieldCode="DE" term="%22Geology%22">Geology</searchLink>
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  Data: The 300±20 Ma anomalously radioactive trachytes of Wadi El Kareim, central Eastern Desert, are a significant example of U‐mineralization related to the alkaline volcanics in Egypt. Extensive portable gamma‐ray spectrometric data has been utilized to identify geological factors controlling uranium mobility in the geological units along the three detailed study locations of Kab Al‐Abyad, South Wadi (W) Al‐Tarafawy and W. Al‐Farkhah; their eTh/eU ratios averaging around 4.1, 3.7 and 5.6 respectively. Quantitative analysis with the integration of mobility maps and geological studies suggest two systems controlling U‐migration within the geological units (confined system and unconfined system). In the confined system, the syngenetically formed U have experienced mobility after leaching and are redistributed in the presence of an incorporation carrier during transportation (probably as carbonate complexes). Then the retardant for uranium is achieved by sorption or by coprecipitation with the aid of Fe oxy‐hydroxide, and finally the formation of immobile secondary U‐bearing minerals takes place along a lithogeochemical trap. In contrast to the confined system, the unconfined one is basically lacking the lithogeochemical trap which influences the final accumulation of U‐bearing minerals. The radioactivity of the trachyte rocks arises from the radioactive minerals uranophane and beta‐uranophane with U‐ and/or Th‐bearing minerals samarskite, Th‐rich REE silicates, monazite and allanite. [ABSTRACT FROM AUTHOR]
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        Value: 10.1111/1755-6724.13724
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      – Code: eng
        Text: English
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        PageCount: 19
        StartPage: 2214
    Subjects:
      – SubjectFull: Migration of uranium
        Type: general
      – SubjectFull: Gamma ray spectrometry
        Type: general
      – SubjectFull: Radioactivity
        Type: general
      – SubjectFull: Geochemistry
        Type: general
      – SubjectFull: Volcanism
        Type: general
      – SubjectFull: Geology
        Type: general
      – SubjectFull: Egypt
        Type: general
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      – TitleFull: Using Portable Gamma‐Ray Spectrometry for Testing Uranium Migration: A Case Study from the Wadi El Kareim Alkaline Volcanics, Central Eastern Desert, Egypt.
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            NameFull: DESSOUKY, Osama K.
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            NameFull: ALI, Hani H.
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              M: 12
              Text: Dec2018
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              Y: 2018
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