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Hydrothermally Altered and Fractured Granite Hosting Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt

Received: 22 August 2014     Accepted: 26 August 2014     Published: 17 September 2014
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Abstract

Gabal Adara Adatalob granite in the south Eastern Desert, Egypt represents a promising example for hydrothermally altered and fractured granite hosting rare metals and rare earths mineralization. This granite host or act as a source for the rare metals (Zr, Y, Nb, Yb and Ga) and rare earths (La, Ce, Pr, Nd, Sm, and Yb) mineralization. It forms isolated pluton crop out in the wadi Ed Direira area. It shows highly alteration and a strong enrichment in some rare metals and rare earths contents (Zr = 1434, Y = 629, Nb = 258, Ga =39, La = 262.18, Ce = 546, Pr = 71.91, Nd = 366.88, Sm = 101. 46, Yb = 8.12 ppm). Field radiometric measurements for this granite revealed that low uranium and thorium content. The radioactivity level reaches up to 10.1 ppm (eU), 24.2 ppm (eTh) respectively. The chondrite normalized rare earth elements, trends indicate strongly fractioned rare earth element pattern with significant strong enrichment in light rare earth elements rather than heavy rare earth elements.

Published in Earth Sciences (Volume 3, Issue 6-1)

This article belongs to the Special Issue Hydrothermally Altered and Fractured Granite Host Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt

DOI 10.11648/j.earth.s.2014030601.11
Page(s) 1-7
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2014. Published by Science Publishing Group

Keywords

Hydrothermally Altered, Gabal Adara Adatalob, Rare Metal, Eastern Desert

References
[1] Ball, J. (1912):The geography and geology of south eastern Egypt. Geol. Surv., Cairo. P. 394.
[2] Hume, W.F. (1935): Geology of Egypt. II. The fundamental Precambrian rocks of Egypt and Sudan: Part I, The metamorphic rocks : 1 – 300, Part II, The later plutonic and minor intrusive rocks : 301- 688, Part III, The minerals of economic value : 689 – 900, Geol. Surv. Egypt.
[3] Egyptian Geological Survey, (2002): Marsa Shaab Quadrangle map, Scale, 1:250,000. Geol. Surv. Egypt, Cairo.
[4] Hussein, I. M. (1977): Geology of the Halaib area of the northern Red Sea Hills, Sudan, with reference to the Sol Hamed basic complex. M. Sc., Portsmouth Polytechnic, England.
[5] Fitches, W.R.; Graham , R.H.; Hussein, I.M.;Ries, A.C.; Shackleton, R.M. and Rice, R.C. (1983): The Late Proterozoic affiliate of Sol Hamed, NE Sudan Precambrian Research, V. 19, PP. 385 – 41 , Elsevier Amsterdam.
[6] El Alfy, Z.; Bagddady, M.; Awaga, G.; Morsei, A.; Ramadan, T. and Abdallah, M. A. 1994. Geochemical exploration of Elba – Gerf area south Eastern Desert, Egypt, Geol. Surv., Cairo (unpublished report ).
[7] Nasr, B.B. and Youssef, M. 1995. New occurrences of Tertiary alkaline rocks at Gebel Elba area South Eastern Desert, Egypt. Annals of Geol. Surv. V. XX. . PP.871 – 873.
[8] 8] Khalaf I.M. (2005): Geology of the area around G. Qash Amir with special emphases on the granitic rocks, south Eastern Desert, Egypt. Egypt J Geol 49:49–64
[9] Omar, M. A.; Said, S. M.; Morsi, A. M. and Abu EL Labn, S. A. (1998): Geochemical map sheet No. 36 NE L 1,2,3 Qash Amir area, south Eastern Desert, Egypt. Geol. Surv. , Cairo ( unpublished report ).
[10] Shahin A.A. (2011): Occurrence of uraniferous iron and manganese oxides in biotite granite North East Gabal El Sela area, South Eastern Desert, Egypt. Arabian Journal of Geosciences , Vol. 6, Issue 7, pp 2245-2259.
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    Hassan Abd El Razek Aly Shahin, Masoud Salah Masoud. (2014). Hydrothermally Altered and Fractured Granite Hosting Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt. Earth Sciences, 3(6-1), 1-7. https://doi.org/10.11648/j.earth.s.2014030601.11

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    ACS Style

    Hassan Abd El Razek Aly Shahin; Masoud Salah Masoud. Hydrothermally Altered and Fractured Granite Hosting Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt. Earth Sci. 2014, 3(6-1), 1-7. doi: 10.11648/j.earth.s.2014030601.11

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    AMA Style

    Hassan Abd El Razek Aly Shahin, Masoud Salah Masoud. Hydrothermally Altered and Fractured Granite Hosting Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt. Earth Sci. 2014;3(6-1):1-7. doi: 10.11648/j.earth.s.2014030601.11

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  • @article{10.11648/j.earth.s.2014030601.11,
      author = {Hassan Abd El Razek Aly Shahin and Masoud Salah Masoud},
      title = {Hydrothermally Altered and Fractured Granite Hosting Rare Metal at Gabal Adara Adatalob, South Eastern Desert, Egypt},
      journal = {Earth Sciences},
      volume = {3},
      number = {6-1},
      pages = {1-7},
      doi = {10.11648/j.earth.s.2014030601.11},
      url = {https://doi.org/10.11648/j.earth.s.2014030601.11},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.s.2014030601.11},
      abstract = {Gabal Adara Adatalob granite in the south Eastern Desert, Egypt represents a promising example for hydrothermally altered and fractured granite hosting rare metals and rare earths mineralization. This granite host or act as a source for the rare metals (Zr, Y, Nb, Yb and Ga) and rare earths (La, Ce, Pr, Nd, Sm, and Yb) mineralization. It forms isolated pluton crop out in the wadi Ed Direira area. It shows highly alteration and a strong enrichment in some rare metals and rare earths contents (Zr = 1434, Y = 629, Nb = 258, Ga =39, La = 262.18, Ce = 546, Pr = 71.91, Nd = 366.88, Sm = 101. 46, Yb = 8.12 ppm). Field radiometric measurements for this granite revealed that low uranium and thorium content. The radioactivity level reaches up to 10.1 ppm (eU), 24.2 ppm (eTh) respectively. The chondrite normalized rare earth elements, trends indicate strongly fractioned rare earth element pattern with significant strong enrichment in light rare earth elements rather than heavy rare earth elements.},
     year = {2014}
    }
    

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    AU  - Hassan Abd El Razek Aly Shahin
    AU  - Masoud Salah Masoud
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    UR  - https://doi.org/10.11648/j.earth.s.2014030601.11
    AB  - Gabal Adara Adatalob granite in the south Eastern Desert, Egypt represents a promising example for hydrothermally altered and fractured granite hosting rare metals and rare earths mineralization. This granite host or act as a source for the rare metals (Zr, Y, Nb, Yb and Ga) and rare earths (La, Ce, Pr, Nd, Sm, and Yb) mineralization. It forms isolated pluton crop out in the wadi Ed Direira area. It shows highly alteration and a strong enrichment in some rare metals and rare earths contents (Zr = 1434, Y = 629, Nb = 258, Ga =39, La = 262.18, Ce = 546, Pr = 71.91, Nd = 366.88, Sm = 101. 46, Yb = 8.12 ppm). Field radiometric measurements for this granite revealed that low uranium and thorium content. The radioactivity level reaches up to 10.1 ppm (eU), 24.2 ppm (eTh) respectively. The chondrite normalized rare earth elements, trends indicate strongly fractioned rare earth element pattern with significant strong enrichment in light rare earth elements rather than heavy rare earth elements.
    VL  - 3
    IS  - 6-1
    ER  - 

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Author Information
  • Nuclear Materials Authority, P. O. Box 530, El-Maadi, Cairo, Egypt

  • Nuclear Materials Authority, P. O. Box 530, El-Maadi, Cairo, Egypt

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