Titlebook: Ediacaran-Paleozoic Rock Units of Egypt; Their Correlation wi Mohamed Abdel Ghany Khalifa Book 2023 The Editor(s) (if applicable) and The A

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alents rock units in Libya, Jordan, Saudi Arabia and Iraq. A paleogeographic map has been drawn all over the studied countries to manifest the facies changes and the possible depositional environment.

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positional environments of the Permian rock units. The depositional environments of Egyptian rock units and their equivalent rock units in adjacent countries are interpreted using lithological types and faunal and floral associations.

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Conspiracy

The Ediacaran Rock Units,mmamat and the El Urf formations) belong to the Ediacaran Neoproterozoic, while the third (Abu Haswa Formation) belong to the Ediacaran sedimentary rocks. The Hammamat Formation refers to the Ediacaran clastic rocks found in an isolated basin within the Neoproterozoic rocks of Egypt’s central Easter

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The Cambrian Period,ora, palaeogeography, and tectonic events that occurred during this period. It describes two rock units in Egypt: the Middle Cambrian Araba Formation, which is visible on the surface, and the Shifa Formation, which is found in the subsurface at the Siwa basin in the northwestern Desert. This chapter

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The Silurian Period, which are found in the subsurface in the Siwa basin in the northwestern Desert. The Um Ras formation is found in the Um Ras Plateau, northeast of Gebel Uweinat. It comprises a non-cyclic sequence of pale reddish massive sandstone with thin intercalations of horizontally bedded sandstone enriched wi

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泰然自若

The Carboniferous Period,l and floral associations, and other information. It is concerned with the Carboniferous rock units of Egypt and neighbouring countries. Lower Carboniferous rock units include the Umm Bogma and Abu Thora formations in southwest Sinai and the Wadi Malik Formation in the Gilf plateau in the southweste