2021
DOI: 10.1007/s12517-021-09141-5
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Geochemistry and paleoweathering of metasediments and pyrite-bearing quartzite during the Neoproterozoic Era, Wadi Ibib-Wadi Suwawrib, South Eastern Desert, Egypt

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Cited by 22 publications
(12 citation statements)
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“…Younger granitic rocks are abundant in Central Eastern Desert of Egypt relative to the southern part [2,10,17]. Multi magmatic phases of Homrit Waggat area lie ~50 km NW of Mersa Alam town (Figure 1a) that have been discussed by many authors, such as Azer et al [10].…”
Section: Geologic Settingmentioning
confidence: 87%
“…Younger granitic rocks are abundant in Central Eastern Desert of Egypt relative to the southern part [2,10,17]. Multi magmatic phases of Homrit Waggat area lie ~50 km NW of Mersa Alam town (Figure 1a) that have been discussed by many authors, such as Azer et al [10].…”
Section: Geologic Settingmentioning
confidence: 87%
“…Crystalline rocks of Egypt, which are dominantly distributed in the Eastern Desert and South Sinai as well as the Uwainate area, constitute the northern sector of the Arabian Nubian Shield (ANS) [ 18 , 19 , 20 ]. These rocks include infrastructure gneisses, ophiolite and arc assemblages, and variable compositions of granitic intrusion [ 21 , 22 , 23 , 24 ]. ANS represents the main crustal juvenile that developed during the late Proterozoic Era by closing the Mozambique Ocean [ 19 , 21 ], exposed from Egypt to Ethiopia on the Nubian side and from Saudi Arabia to Yemen on Arabian Side [ 25 ].…”
Section: Introductionmentioning
confidence: 99%
“…These rocks include infrastructure gneisses, ophiolite and arc assemblages, and variable compositions of granitic intrusion [ 21 , 22 , 23 , 24 ]. ANS represents the main crustal juvenile that developed during the late Proterozoic Era by closing the Mozambique Ocean [ 19 , 21 ], exposed from Egypt to Ethiopia on the Nubian side and from Saudi Arabia to Yemen on Arabian Side [ 25 ]. Syn-, late- and post-orogenic granitic rocks of Late Cryogenian–Ediacaran are widely distributed in ANS, covering about sixty percent of the Egyptian Neoproterozoic rocks [ 26 ].…”
Section: Introductionmentioning
confidence: 99%
“…Igla mine area locates in the CED of Egypt (Fig. 4 a) and is dominated by metavolcanics, older granites, and biotite pink granites 31 , 32 . The metavolcanics rocks are well exposed in the southern part of the study area (Fig.…”
Section: Geologic Settingmentioning
confidence: 99%