Pore Fabric Anisotropy of the Cambrian–Ordovician Nubia Sandstone in the Onshore Gulf of Suez, Egypt: A Surface Outcrop Analog

Author:

Elgendy Nader T. H.,Abuamarah Bassam A.,Nabawy Bassem S.,Ghrefat Habes,Kassem Osama M. K.

Funder

Deanship of Scientific Research, King Saud University

Publisher

Springer Science and Business Media LLC

Subject

General Environmental Science

Reference84 articles.

1. Abdallah, A. M., & Adindani, A. (1963). Stratigraphy of Upper Paleozoic rocks, western side of the Gulf of Suez (Vol. 25). Egypt: Geological Survey and Mineral Resource Department.

2. Abdallah, A. M., Darwish, M., El Aref, M., & Helba, A. A. (1992a). Lithostratigraphy of the pre-Cenomanian clastics of north Wadi Qena, Eastern Desert, Egypt. In A. Sadek (Ed.), Proceedings of the first international conference on Geology of the Arab World (pp. 255–282). Cairo: Cairo University.

3. Abdallah, A. M., El Aref, M. M., & Helba, A. A. (1992b). Lithostratigraphy of the pre-Cenomanian clastics of north Wadi Qena, Eastern Desert, Egypt. In Proceedings of the second international conference on Geology of the Arab World (pp. 255–282). Cairo University, Cairo.

4. Abdel-Wahab, A. A. (1988). Lithofacies and diagenesis of the Nubia Formation at Central Eastern Desert, Egypt. In 9th EGPC Expl. Conf., Cairo, 9.

5. Abdel-Wahab, A. A. (1998). Diagenetic history of Cambrian quartz arenite, Ras Dib-Zeit Bay area, Gulf of Suez, Eastern Desert, Egypt. Sedimentary Geology,121(1), 121–140.

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