Sequence stratigraphy and depositional environments of Late Cretaceous–Early Palaeogene succession, North Eastern Desert, Egypt

2015 ◽  
Vol 108 (2-3) ◽  
pp. 345-359 ◽  
Author(s):  
Mohamed Youssef ◽  
Mahmoud Hefny
Keyword(s):  
Sequence Stratigraphy ◽  
Late Cretaceous ◽  
Eastern Desert ◽  
Depositional Environments ◽  
North Eastern

Sequence stratigraphy of the Cenomanian Galala Formation, north Eastern Desert, Egypt

2014 ◽  
Vol 89 ◽  
pp. 133-148 ◽  
Author(s):  
M.A. Khalifa ◽  
Mohamed S. Abu El-Ghar ◽  
S.A. Helal ◽  
A.W. Hussein
Keyword(s):  
Sequence Stratigraphy ◽  
Eastern Desert ◽  
North Eastern

Late Cretaceous Kholokhovchan floral assemblage of the Okhotsk-Chukotka volcanogenic belt (North-Eastern Asia)

Palaeobotany ◽  
2013 ◽  
Vol 4 ◽  
pp. 116-147 ◽  
Author(s):  
S. V. Shczepetov ◽  
A. B. Herman
Keyword(s):  
Late Cretaceous ◽  
Eastern Asia ◽  
Plant Fossils ◽  
Volcanogenic Belt ◽  
North Eastern ◽  
Volcanogenic Deposits ◽  
Floral Assemblage ◽  
Eastern Russia ◽  
Comprehensive Study

Results of comprehensive study of the Kholokhovchan floral assemblage collection is summarized. These plant fossils were collected in 1978 by E. L. Lebedev from volcanogenic deposits in Penzhina and Oklan rivers interfluve, North-Eastern Russia. This assemblage was previously known as a list of Lebedev’s preliminary identifi cations only. He had suggested that the Kholokhovchan assemblage is correlative to the latest Albian — early Turonian Grebenka flora from the Anadyr River middle reaches. However, our study demonstrates that the Kholokhovchan assemblage is most similar to the presumably the Turonian-Coniacian Arman flora of the Okhotsk-Chukotka volcanogenic belt and, therefore, should be dated as the Turonian-Coniacian or Turonian.

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