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This document discusses adakitic rocks found in the Pan-African Arabian-Nubian Shield in Egypt. It analyzes the petrological and geochemical properties of volcanic rocks from the Dokhan volcanics in the Eastern Desert of Egypt. The rocks have geochemical signatures indicating melting of mafic lower crust interacting with mantle-derived magma. The volcanics were formed by various processes including partial melting, crystal fractionation, and assimilation.

Author

Lami Noman

Language

EN