Page 29 - Reservoir Formation Damage
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Mineralogy  and Mineral  Sensitivity  of Petroleum-Bearing  Formations  13

                                         Table 2-1
                         Description of the Authigenic Clay Minerals*

             Mineral        Chemical Elements* f             Morphology
             Kaolinite  Al 4[Si 40 10](OH) 8           Stacked  plate or  sheets.
             Chlorite   (Mg,Al,Fe) 12[(Si,Al) 80 20](OH) 16  Plates,  honeycomb,
                                                       cabbagehead rosette or fan.
             Illite                                    Irregular  with  elongated
                                                       spines or granules.
             Smectite   (|Ca, NA) 07(A1, Mg, Fe) 4[(Si, Al) g  Irregular,  wavy, wrinkled
                         0 20] • nH 20                 sheets, webby or honeycomb.
             Mixed      Illite-Smectite                Ribbons substantiated by
             Layer      Chlorite-Smectite              filamentous  morphology.
             *  After Ezzat, ©1990 SPE;  reprinted by permission of the Society of Petroleum Engineers.
             t  After J. E. Welton (1984).












                                                                  SAND-SIZE
                                                                   RITAL GRAIN
                    ISOPACHOUS
                    RIM  CEMENT
                                                                  PORE THROAT
                                                                CEMENT
                    INTERGRANULAR
                       PORES

               DEFORMED  _
             MUD  FRAGMENT
                INTERGRANULAR
                  PRESSURE -                                      MICROPOROSITY
                  SOLUTION                                           IN CLAY


                                INTERGRANULAR
                                    PORE
                                    BODY
             Figure  2-2.  Description  of the  constituents in typical  sandstone  (after  Mancini,
             1991;  reprinted  by  permission  of  the  U.S.  Department  of  Energy).
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