Sediment‐Hosted Mineral Deposits 1990
DOI: 10.1002/9781444303872.ch13
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Syngenetic and Paleokarstic Copper Mineralization in the Palaeozoic Platform Sediments of West Central Sinai, Egypt

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Cited by 20 publications
(9 citation statements)
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“…Eastern Aswan area represents the main occurrence of the Cretaceous ironstone bands of South Egypt, which are confined to clastic successions belonging to the "Nubian" sandstones or "Nubia facies" [17,18]. Three different samples were obtained from different locations from Aswan region.…”
Section: Methodsmentioning
confidence: 99%
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“…Eastern Aswan area represents the main occurrence of the Cretaceous ironstone bands of South Egypt, which are confined to clastic successions belonging to the "Nubian" sandstones or "Nubia facies" [17,18]. Three different samples were obtained from different locations from Aswan region.…”
Section: Methodsmentioning
confidence: 99%
“…[16][17][18], there is a significant shift in the position of the peak maxima in the Fe 2p doublet, the B.E. positions are observed to be at ∼709.48-709.68 eV (for Fe Fig.…”
Section: X-ray Photoelectron Spectroscopy (Xps)mentioning
confidence: 99%
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“…Taba is the northernmost resort of Egypt's Red Sea Riviera, it is a frequent vacation spot for Egyptians and tourists, and it has been declared as a protected area, in 1998. Taba area is a desert and a natural heritage which covers a land area of 3595 km 2 and dates back to 5000 years (EI-Sharkawi et al, 1990;Abdallah, 1992). The area comprises a group of hills (more than 1000 m in height) and a number of water springs (such as Hadra spring in Wadi Ghazala, Oum Ahmed spring in Wadi Elswana, and Fortaga spring in Wadi Water) (EI-Sharkawi et al, 1990;El-Refaei, 1992).…”
Section: Introductionmentioning
confidence: 99%
“…Taba area is a desert and a natural heritage which covers a land area of 3595 km 2 and dates back to 5000 years (EI-Sharkawi et al, 1990;Abdallah, 1992). The area comprises a group of hills (more than 1000 m in height) and a number of water springs (such as Hadra spring in Wadi Ghazala, Oum Ahmed spring in Wadi Elswana, and Fortaga spring in Wadi Water) (EI-Sharkawi et al, 1990;El-Refaei, 1992). Over the last few years the Egyptian government devoted a tremendous effort in planning for the development of Taba in terms of new urbanization, tourism, and mega development projects.…”
Section: Introductionmentioning
confidence: 99%