The Abu Dabbab area is located in the central Eastern Desert of Egypt, this area is covered bu ophiolitic serpentinites, metavolcanics and metasedimens that were intruded by albite granite stock. The normalized REEs pattern of ophiolitic metabasalts indicate N-MORB, whereas the normalized REEs of albite granite and ophiolitic metasediments; mainly feldspathic silt stones are strongly matching for both. Thanks in advance.

MH

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