English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

El GidamiEl Garra area lies between latitudes 26 24– 26 27 N and longitudes 33 20– 33 29 E, in the central Eastern Desert of Egypt, 3 km south of the midpoint of Qena-Safaga highway. The area is covered by younger granites intruded into amphibolites, and syn-tectonic granites. It represents one of the most promising uranium occurrences in the Eastern Desert. The main granitic types forming this pluton as defined from their mineral composition and textures comprise pegmatitic perthite granite, perthite granite and fluorite perthite granite. Petrographically, these three types of younger granites are similar. The three types are perthitic in composition and medium to very coarse grained, even pegmatitic. Quartz, potash feldspar and plagioclase, with small amount of biotite and opaque minerals constitute the mineral assemblage in these types. Fluorite, zircon, allanite, titanite, apatite and monazite are accessory minerals. Chlorite, epidote, saussurite and muscovite are secondary constituents. In addition, there are some important radioactive minerals in the studied granites such as uranophane, xenotime and metamict zircon. Locally, the estimated values of the external absorbed γ-radiation dose rate are 221.4±43.87, 242±51.16, 190.6±56.24 and 294.9±39.81 (nGy/h) for the granitic rocks; fluorite perthite, Syn-tectonic, perthite and pegmatite perthite, respectively. These values are much higher than the worldwide average. Fortunately, neither public activities nor residential centers are recognized around the studied granites at El Gidami area. The activity concentrations of the studied rocks are below the regulated values. As a result, all the occupational activities during surface exploration or transportation of the studied granitic rocks are excluded from the regulations and no need for any recommendations about the resulting effective doses. Generally, the slabs of thickness of 4cm from the different locations and granitic rock types exhibit an annual effective dose up to 2.41 (mSv/y). This value is below the action level and the studied granitic rock types may be used safely as decorative materials.

GEOLOGY, SPECTROMETRY AND EVALUATION OF THE RADIATION EXPOSURES AT EL GIDAMI-EL GARRA AREA, CENTRAL EASTERN DESERT, EGYPT