| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6448397 | Cretaceous Research | 2012 | 19 Pages |
Abstract
⺠Four sedimentary facies were recognized in the Cenomanian-Turonian succession. ⺠The facies are peritidal clastic & carbonates and sallow & deep subtidal facies. ⺠This succession is divided into four sequences delineated by five boundaries. ⺠Sedimentation of the sequences is controlled by local, regional and global factors.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Palaeontology
Authors
Shaban Ghanem Saber,