Page 18 - Geology of Carbonate Reservoirs
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ABOUT THIS BOOK








                          To understand carbonate rocks at reservoir scale, one first has to understand them
               at pore scale. Carbonate reservoirs are porous and permeable rocks that contain
               hydrocarbons. Carbonate porosity includes three end - member genetic categories:
               purely depositional pores, purely diagenetic pores, and purely fracture pores. Inter-
               mediate types exist, of course, but the point is that there are three main types of
               carbonate porosity that represent distinctly different geological processes. Before

               one can fully appreciate these differences and be proficient at distinguishing between
               the varieties of carbonate reservoir types, one must understand what carbonates are,
               how and where they form, and how they become reservoirs. One must understand
               the differences between reservoirs, traps, and seals and learn to appreciate that res-

               ervoir characterization is the study of rocks plus  the fluids they contain. The opera-
               tive word is rocks. Carbonate rocks consist of component particles and maybe some
               lime mud matrix and cement. The skeletal and nonskeletal particles, along with mud
               and cement, hold an enormous amount of information about the depositional and
               diagenetic environments that produced the reservoir rock. This book begins with
               definitions, with discussions about how, where, and why carbonates are formed and

               about how fundamental rock properties are used to create a language for commu-
               nicating information about the rocks — carbonate rock classifi cations.  Reservoir
               porosity and permeability are variables that depend on fundamental rock proper-

               ties. The book explores how rock classifications do or do not correspond with


               conventional porosity classifications. Reservoirs contain fluids; therefore we
               explore reservoir properties such as saturation, wettability, capillarity, and capillary
               pressure.
                    Geophysical (borehole) logs are briefly mentioned because they provide infor-

               mation about third - order rock properties. Logs provide important information to
               develop static and dynamic reservoir models, to calculate fluid properties such as

               saturation and movable oil volumes, to make stratigraphic correlations, and to inter-
               pret lithological characteristics in boreholes where no rock samples are available.
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