الفهرس 
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Abstract
The Presen Work Deals With the Mineralogy and Pertrology of Gabal Qatrani Fayum Provincs Egypt the Study Area was Geologically mapped, (using aerial photographs, scale 1:40,000) and studied from the lithostratigraphical, structural, petrographical Grain Size Analysis Mineralogyical and Geochemical Points of View.
from the map area north of Birket Qarun, the follow’ ng rock units were recognized from top to bottom as:
6. Pliestocene sediments.
The Casr El Sagha Formation is paraconformably ’overlain by the Gabal Qatrani Formation which is composed of several multticoloured heds of sandstone, siltstone, claystone, carbonate and