Page 125 - Geology of Carbonate Reservoirs
P. 125

CHAPTER FIVE
















               DEPOSITIONAL CARBONATE

               RESERVOIRS






                         This chapter focuses on depositional porosity, depositional environments, and depo-
               sitional rock properties. Different depositional environments that exist across ramps
               and shelves produce distinctive depositional successions. The fundamental rock
               properties that characterize each of these depositional successions can be synthe-
               sized to create seven ideal depositional successions . For ease in visualization, each
               ideal depositional succession is described and illustrated to resemble borehole cores.
               Most successions represent shallowing - upward deposition and most of them can be

               divided into several parts (the microfacies defined earlier) to enhance their indi-

               vidual character and make it easier to identify them in the field or in borehole cores.
               Review questions on volumetric calculations, on exploration strategies, and on the

               best methods for field development in different facies are included at the end of the
               chapter and selected case histories of depositional reservoirs are presented in
               Chapter  8 .
                    Depositional reservoirs are those in which reservoir porosity is the result of
               depositional processes only. Older literature might classify this kind of porosity as
                 “ primary. ”  Recognizing depositional reservoirs depends on the ability to distinguish
               depositional porosity from diagenetic and fracture porosity, along with the various
               hybrids of end - member pore types that are usually present. Purely depositional
               porosity is rare but depositional texture, fabric, or mineralogy usually have so much

               influence on diagenesis that altered reservoirs can be exploited as if they were gov-
               erned by depositional porosity only. For example, it is common to fi nd reservoirs
               with fabric - selective, texture - selective, or facies - selective porosity and permeability
               even though the rocks have been altered by diagenesis. These are hybrid reservoirs
               because the pore characteristics reflect both depositional and diagenetic infl uences.


               In order to confirm that hybrid reservoirs have both depositional and diagenetic

               Geology of Carbonate Reservoirs: The Identification, Description, and Characterization of Hydrocarbon
               Reservoirs in Carbonate Rocks
               By Wayne M. Ahr  Copyright © 2008 John Wiley & Sons, Inc.
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