--> Abstract: Sedimentology and Paleogeography of the Natih Carbonate Platform in the Oman Mountains, by J. M. Philip, J. R. Borgomano, and S. Al Maskiry; #90990 (1993).

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PHILIP, J. M., University Aix-Marseille I, Marseille, France; J. R. BORGOMANO and S. AL MASKIRY, Petroleum Development Oman, Muscat, Oman

ABSTRACT: Sedimentology and Paleogeography of the Natih Carbonate Platform in the Oman Mountains

Field study of the Natih Formation in the Jebel Akhdar and the Oman foothills allows us to establish a new stratigraphical and sedimentological model of this important hydrocarbon reservoir unit. Thanks to the study of rudists and the discovery of ammonites, new precisions can be given to the chronostratigraphy of the Natih Formation. It was especially demonstrated by the presence of Hippuritids (rudists) that the top of the Natih Formation matches the Cenomanian/Turonian boundary and corresponds to either rudist-rich layers or hard grounds and condensed levels.

The stratigraphical correlations between several outcrop sections allow one to establish a conceptual sequence stratigraphic model, which can be compared to the subsurface by using the Natih subdivisions "A to G." The recognition of sequence boundaries, maximum flooding surfaces, and system tracts might help to understand the seismo-stratigraphic expression of the Natih interval in the subsurface. Furthermore, this sequence stratigraphic model clearly illustrates the interfingering of the carbonate reservoir intervals and the organic-rich units (Fitri Mb) at the top of the Natih Formation.

We also have identified a clear zonation from deeper marine to shallow-marine carbonate deposits, the most significant of which are the rudistid facies. They form banks, thickets, and biostroms and do not constitute anomalous build ups such as bioherms. Good leaching potentials generally are related to these rudistid facies, especially when they are very rich in skeletal aragonite from the Caprinids shells. Significant primary porosity may be related also to the Hippuritid skeletal cavities at the top of the Natih. Reservoir potentials can be enhanced if these Caprinid-rich intervals are related to exposure surfaces such as the top Natih E and the top Natih A.

AAPG Search and Discovery Article #90990©1993 AAPG International Conference and Exhibition, The Hague, Netherlands, October 17-20, 1993.