Facies architecture and controlling factors induced depositional model of the Quaternary carbonate eolianites in the northwestern Mediterranean coast of Egypt

Author:

Assal Ehab M.ORCID,Abdel-Fattah Zaki. A.,El-Asmar Hesham M.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference78 articles.

1. Abdel-Fattah ZA, Kora MA, Ayyad SN (2013) Facies architecture and depositional development of Middle Miocene carbonate strata at Siwa Oasis, northwestern Egypt. Facies 59:505–528

2. Abegg FE, Harris PM, Loope DB (2001) Modern and ancient carbonate eolianites. Sedimentology, sequence stratigraphy, and diagenesis. Society of Sedimentary Geology Special Publication, Tulsa

3. Acharya B, Bhatt N (2019) Sedimentological analysis of a late quaternary coastal dune system: an example from gopnath, south-east Saurashtra, Western India. Sedimentology 66:435–458

4. Ali YA, West I (1983) Relationship of modern gypsum nodules in sabkhas of loess to compositions of brines and sediments in northern Egypt. J Sediment Petrol 53:1151–1168

5. Attia SH, El-Ghazawy M (1984) Microfacies studies on some Tertiary and Quaternary deposits east of El-Hammam NW Desert. Egypt Middle East Research Centre Ain Shams Univ 4:239–273

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