Article ID Journal Published Year Pages File Type
4728933 Journal of African Earth Sciences 2013 16 Pages PDF
Abstract
► The studied rocks were deposited on a ramp. ► Four third-order depositional sequences were recorded. ► The main factor controlling distribution of facies is change in the relative sea level. ► The oceanic anoxic event is placed around the Cenomanian-Turonian boundary.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
Depositional environments and sequence architecture of the Raha and Abu Qada formations (Cenomanian-Turonian), west central Sinai, Egypt
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