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The volcano‐sedimentary succession around Wadi Zaghra in Sinai, at the northernmost segment of the Arabian Nubian Shield, comprises volcanic rocks interbedded with rather immature sediments. The succession is dominated by intermediate to silicic volcanics of medium‐ to high‐K calc‐alkaline affinity. It is divided into two units, the lower unit includes intermediate rocks and dacites interbedded with...
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