Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Youssef S. Bazeen"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-16 (2024)
Abstract The Late Cretaceous was a time of high eustatic sea level that enabled extensive epicontinental seaways and carbonate platforms across the Tethyan Realm, providing favorable habitats for oyster communities to flourish. This study focuses on
Externí odkaz:
https://doaj.org/article/c3ccef6cac784fa9a098e00e442e5338
Autor:
Sherif Farouk, Sreepat Jain, Fayez Ahmad, Tamer Abu-Alam, Khaled Al-Kahtany, Ibrahim S. El Agroudy, Youssef S. Bazeen, Fatma Shaker
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Forty-three planktic foraminifera samples from the Themed section (East Central Sinai; Egypt) spanning the Zone Parvularugoglobigerina eugubina (Pα) to the Subzone Acarinina subsphaerica (P4b) have been studied. Data from δ13C, δ18O, and planktic
Externí odkaz:
https://doaj.org/article/58d1566a7fd144dda2ce5f59732d28e8
Publikováno v:
International Journal of Earth Sciences. 112:1091-1112
The Egyptian lower Eocene carbonate rocks (Thebes Formation) are part of an extensive carbonate platform formed during an eustatic regression along the Tethyan Ocean's southern margin. These rocks are essential in developing Egypt's petroleum system
Publikováno v:
Geological Journal. 58:264-282
Autor:
Youssef S. Bazeen, Abdel Galil A. Hewaidy, Ahmed Samir, El Sayed M. Moneer, Mohamed W. Abd El-Moghny, Haitham M. Ayyad
Publikováno v:
Palaeoworld.
Publikováno v:
Historical Biology. 33:3530-3541
The Maastrichtian sedimentary succession in the Abu Monqar-west Dakhla stretch yields rare cephalopod content. Six cephalopods, including three nautiloids and three ammonoids, are described in deta...
Autor:
Mohammad Haddadi, Mohammad Vahidinia, Mohamad Hosein Mahmudy Gharaie, Meysam Shafiee Ardestani, Youssef S. Bazeen, Dalila Zaghbib-Turki
Publikováno v:
Journal of African Earth Sciences. 200:104889
Publikováno v:
Cretaceous Research. 138:105291
Publikováno v:
Cretaceous Research. 137:105247
Publikováno v:
Geological Journal. 55:4375-4397