Page 236 - Carbonate Facies in Geologic History
P. 236

Facies Sequence in the Permian Reef Complex                       223

               Table VIII-1 (continued)
               General facies   Wilson's facies belt   Tyrell (1969), Dunham (1972) microfacies
               name (Meissner,   number and name   designation
               1972)

               Carlsbad       6. Winnowed platform   Winnowed  shelf  sand;  skeletal  lithoclastic
                                edge sands         dolomite grainstone, with coated grains,
                                                  foraminifera, dasycladacean algae, ooids,
                                                  thick-shelled gastropods, cross-bedded  lime
                                                   sand. (Many marine to meteoric vadose sedi-
                                                  mentary-diagenetic features.)

               Capitan        5. Organic reef of   Shelf edge carbonate; lithoclastic skeletal
                                platform margin   lime  grainstone  and  wackestone;  bioclastic
                                                  debris mixed with lime mud or silt and
                                                  boundstone of abundant sessile benthos and
                                                  encrusting biota. Bryozoans, red algae,
                                                   Tubiphytes, foraminifera, sponges,
                                                  brachiopods, crinoids. (Many marine to
                                                  meteoric vadose sedimentary-diagenetic
                                                  features,  e.g.,  large  druse-lined  cavities,  col-
                                                  lapsed  beds,  large  veins  filled  with  coarse
                                                  calcite druse.)


               Capitan        4. Foreslope facies of   Basin slope carbonates; breccia or "reef
                                carbonate platform   tal us;" vague and inclined beds with boulders
                                (marine talus)    and  redeposited fossils.  Finer  grained  beds
                                                  are  lithoclastic-skeletal  wackestones,  partly
                                                  dolomitized

               Delaware facies.   3. Deep shelf margin  or   Basin margin carbonates; dark well-bedded
               Thick tongues of   basin  margin  "toe  of  lithoc1astic skeletal wackestone-packstone,
               limestone inter-  slope"           some very fine-grained. Finer bioclastic
               calated with  fine                 debris  includes  foraminifera  and  abundant
               sandstones (some                   pieces of organisms living up the slope;
               mega-boulder                       almost all are redeposited. Brachiopods,
               beds)                              bryozoans and crinoids prominent. Many
                                                  sedimentary structures including inclined
                                                  foresets, slumps, boulder beds, channels, load
                                                  casts, carbonate mounds


               Delaware facies.   1. Basin        Basinal carbonate; black well-bedded, platy,
               Thin carbonate                     laminated micrograded, fine-grained
               units intercalated                 wackestone-packstone with sponge spicules,
               with fine                          globular foraminifera and radiolarians,
               sandstone                           ammonoids

               Delaware facies,   1. Basin         Starved  basin,  dark  radioactive  silty  shale
               black shale                         with carbonate beds a few cm. thick
               withinfme
               sandstone
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