The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt

The hydrothermal uranium and some other metal deposits occur within the zone of the major NW-SE trending normal fault and its associated minor normal faults that cut the Miocene clastic-carbonate sediments at Ochre-Um Greifat and Wadi Wizr locations. Samples from these locations were subjected to mi...

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Main Authors: Soliman Abu Elatta Abdallah Mahmoud, Gehad Mohammed Reda Mansour
Format: Article
Language:English
Published: SpringerOpen 2018-12-01
Series:Beni-Suef University Journal of Basic and Applied Sciences
Online Access:http://www.sciencedirect.com/science/article/pii/S2314853518303743
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spelling doaj-5f9e22050d3047f4ab7db29f7e4048322020-11-25T01:34:30ZengSpringerOpenBeni-Suef University Journal of Basic and Applied Sciences2314-85352018-12-0174752766The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, EgyptSoliman Abu Elatta Abdallah Mahmoud0Gehad Mohammed Reda Mansour1Corresponding author.; Nuclear Materials Authority, EgyptNuclear Materials Authority, EgyptThe hydrothermal uranium and some other metal deposits occur within the zone of the major NW-SE trending normal fault and its associated minor normal faults that cut the Miocene clastic-carbonate sediments at Ochre-Um Greifat and Wadi Wizr locations. Samples from these locations were subjected to mineralogical and geochemical studies in order to determine their concentrations of strategic and economic elements (e.g., U, Th, Mo, Zn, Pb, As and V) as well as their petrogenesis. The mineralogical studies were confirmed by X-ray diffraction (XRD) and the environmental scanning electron microscopy coupled with energy dispersive spectroscopy ESEM/EDX. The geochemical data was determined by ICP-MS and ICP-OES (Acme Lab. of Canada). The results showed that the Ochre-Um Greifat deposits are enriched in U and Zn elements, with significant concentrations of Cu and Th while Wadi Wizr deposits are enriched in Mo, Zn, Pb and As elements. The discrimination diagrams based on major and trace elements indicated that the Ochre-Um Greifat and Wadi Wizr deposits are of hydrothermal origin. Additionally, uranium deposit was subjected to the supergene processes. Moreover, radionuclides showed that the state of disequilibrium as a result of physicochemical conditions of the hydrothermal solutions and the nature of ambient rocks. The study concluded that the locations need further geological and geophysical studies to determine if nuclear materials (uranium and molybdenum) and other associated elements are economically valuable. Keywords: Hydrothermal deposits, Ochre, Strategic and economic elements, Disequilibriumhttp://www.sciencedirect.com/science/article/pii/S2314853518303743
collection DOAJ
language English
format Article
sources DOAJ
author Soliman Abu Elatta Abdallah Mahmoud
Gehad Mohammed Reda Mansour
spellingShingle Soliman Abu Elatta Abdallah Mahmoud
Gehad Mohammed Reda Mansour
The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
Beni-Suef University Journal of Basic and Applied Sciences
author_facet Soliman Abu Elatta Abdallah Mahmoud
Gehad Mohammed Reda Mansour
author_sort Soliman Abu Elatta Abdallah Mahmoud
title The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
title_short The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
title_full The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
title_fullStr The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
title_full_unstemmed The hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the Red Sea, Central Eastern Desert, Egypt
title_sort hydrothermal uranium and some other metal deposits of the extensional faulting during the advanced opening of the red sea, central eastern desert, egypt
publisher SpringerOpen
series Beni-Suef University Journal of Basic and Applied Sciences
issn 2314-8535
publishDate 2018-12-01
description The hydrothermal uranium and some other metal deposits occur within the zone of the major NW-SE trending normal fault and its associated minor normal faults that cut the Miocene clastic-carbonate sediments at Ochre-Um Greifat and Wadi Wizr locations. Samples from these locations were subjected to mineralogical and geochemical studies in order to determine their concentrations of strategic and economic elements (e.g., U, Th, Mo, Zn, Pb, As and V) as well as their petrogenesis. The mineralogical studies were confirmed by X-ray diffraction (XRD) and the environmental scanning electron microscopy coupled with energy dispersive spectroscopy ESEM/EDX. The geochemical data was determined by ICP-MS and ICP-OES (Acme Lab. of Canada). The results showed that the Ochre-Um Greifat deposits are enriched in U and Zn elements, with significant concentrations of Cu and Th while Wadi Wizr deposits are enriched in Mo, Zn, Pb and As elements. The discrimination diagrams based on major and trace elements indicated that the Ochre-Um Greifat and Wadi Wizr deposits are of hydrothermal origin. Additionally, uranium deposit was subjected to the supergene processes. Moreover, radionuclides showed that the state of disequilibrium as a result of physicochemical conditions of the hydrothermal solutions and the nature of ambient rocks. The study concluded that the locations need further geological and geophysical studies to determine if nuclear materials (uranium and molybdenum) and other associated elements are economically valuable. Keywords: Hydrothermal deposits, Ochre, Strategic and economic elements, Disequilibrium
url http://www.sciencedirect.com/science/article/pii/S2314853518303743
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