skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Carbonate lithofacies, diagenesis, porosity relationships and crude oil geochemistry, Ratawi Formation, Kuwait-Saudi Arabia divided neutral zone

Miscellaneous ·
OSTI ID:7017931

The Neocomian Ratawi Formation, in Kuwait-Saudia Arabia Divided Neutral Zone, is divided into six lithologic facies: algal wackestone (Ia), skeletal wackestone/packstone (Ib), algal boundstone (IIa), biopelpackstone/grainstone (IIb), oobiopelgrainstone (IIc), and planktonic-fossil assemblage indicate a shallow, open normal marine environment. Intermicrite porosity is the dominant porosity in Wafra, Hout and Dorra fields (70-90% of the total 20%) while biomoldic porosity is dominant in Khafji area. The Wafra limestone is interrupted by a long interval of clay invasion which deposited shale/limestone intercalation in the subtidal environment. The total thickness of the boundstone facies ranges from 50-100 feet in Wafra and Khafji to 20 feet in Dorra. The oil was accumulated in three major types of voids; intergranular, biomoldic, and interframe porosities. The biopelpackstone/grainstone (IIb) facies occurs as thick beds in Wafra and Khafji limestones and decreases abruptly in the Hout and Dorra areas. This facies indicates a subtidal/shelf edge depositional environment. This facies exhibits the highest effective porosity (up to 30%), where the dominant biomoldic and intergranular porosities are filled partially with dead oil. The oobiopelgrainstone was confirmed only in the Wafra area where it reaches a thickness of 150 feet. It is composed mainly of coated bioclastic fragments, which indicate an outer shelf depositional environment. The porosity is predominantly intergranular (12-18%) and is filled with oil.

Research Organization:
Texas Tech Univ., Lubbock, TX (USA)
OSTI ID:
7017931
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English