Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Soliman Abu Elatta A. Mahmoud"'
Publikováno v:
Beni-Suef University Journal of Basic and Applied Sciences, Vol 7, Iss 4, Pp 752-766 (2018)
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.
Externí odkaz:
https://doaj.org/article/5f9e22050d3047f4ab7db29f7e404832
Publikováno v:
Acta Geologica Sinica - English Edition. 95:1183-1198
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01e532b28b8c6f5815bc9d5567c6d2e9
https://doi.org/10.1111/1755-6724.14740
https://doi.org/10.1111/1755-6724.14740
Publikováno v:
Geologos, Vol 26, Iss 3, Pp 181-197 (2020)
Unusual deposits formed by corundum are described from two separate pegmatitic veins in the Hafafit-Nugrus area of the South Eastern Desert of Egypt. Other related minerals are described too. The vein-type of corundum at Locality 1 (Vein 1) crosscuts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e61c7825dd98edcff89c29333b55d5de
https://hdl.handle.net/10593/25989
https://hdl.handle.net/10593/25989
Publikováno v:
Minerals & Metallurgical Processing. 35:230-240
The high-grade Th-U-Y zone is one of the numerous mineralized zones found in the El Garra El Hamra hydrothermally altered syenites in southwestern Egypt. It is characterized by the thorium minerals thorite and thorogummite, which are closely associat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::acd83b8c6e215849b331c7a7e2f80ed2
https://doi.org/10.19150/mmp.8600
https://doi.org/10.19150/mmp.8600
The Zug El Bohar hydrothermal uranium-base metal deposits, southwest El Quseir, Red Sea Coast, Egypt
Publikováno v:
Arab Journal of Nuclear Sciences and Applications. 51:228-247
The Zug El Bohar area belongs to the Red Sea coastal plain of Egypt. Lithostratigraphically, this area is represented by a section of Late Cretaceous-Late Miocene sedimentary rocks and it is affected by both a WNW-ESE sinistral strike-slip fault and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e281bd008dc12b8d0230aa81efe449d
https://doi.org/10.21608/ajnsa.2018.3801.1091
https://doi.org/10.21608/ajnsa.2018.3801.1091
Publikováno v:
Ore Geology Reviews. 101:609-628
The El Garra El Hamra complex is a small high-level plug (with associated volcanics) that was emplaced along an ENE-WSW trending dextral strike-slip fault corresponding to the Guinean-Nubian lineament. Owing to continued movement along this fault, th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39ce86537bf187075315442328dc3074
https://doi.org/10.1016/j.oregeorev.2018.08.001
https://doi.org/10.1016/j.oregeorev.2018.08.001
Publikováno v:
Journal of Earth System Science. 128
The Gabal El Faliq area is located in the Eastern Desert of Egypt and belongs to the Wadi Hafafit–Wadi Ghadir fold belt. Lenses and dykes of rare metal-bearing pegmatites occur along major weak zones in the area (Wadi El Gemal strike-slip and its R
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8143a39804ebf9df2c810f9c7c6a8e9
https://doi.org/10.1007/s12040-019-1169-7
https://doi.org/10.1007/s12040-019-1169-7
Publikováno v:
Arabian Journal of Geosciences. 11
Igneous rocks of Nusab El Balgum are formed as an elongated complex mass covering an area of about 4 km × 12.5 km (50 km2), in the NNE-SSW direction of the Tarfawi-Qena-South Sinai trend, which is a branch of the Trans-African shear zone at the inte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ca4d9d17778871ea9dcdb8055855455
https://doi.org/10.1007/s12517-018-3882-y
https://doi.org/10.1007/s12517-018-3882-y