Page 373 - Carbonate Facies in Geologic History
P. 373

360                                                          Summary



                                SEAS
                I                                                    LAGOO'lAL   T I DE
                                                                  CYCLIC SEDIMENTS   FLATS
                FORESLDPE TAWS
                                        PROFILE - 2° TO  25°
                                       ~         .'
                 SEAS  OUIET TO  MODERATE   ~.  ~::.-. :' ~_
                                                            lAOODNAL  CYCLIC SEDIMENTS

                IT                       LOWER  PROFILE



                    ROUGH  SEAS
                                                                  LAGOONAL  MUD   TIDE
                                                                                FLAT
                ill                 STEEPEST PROfiLE-UP TO 45° OR  MORE



               Fig.XII-3. Three types of carbonate shelf margins: I, downslope lime-mud accumulation; II,
               knoll reef ramp or platform; III, organic reef rim. From Wilson (1974, Fig. 1), with permission
               of American Association of Petroleum Geologists



               tense heat and aridity is common, at least seasonally. Marine flooding is sporadic.
               The addition of gypsum or anhydrite, formed from evaporative concentration of
               sea water in  the sediments, is  both depositional and diagenetic.  Precipitation  in
               and replacement of the original sediment occurs as the dense brines move down
               through the sediment or are pulled to the surface through evaporation of intersti-
               tial waters. The precipitated sulfate is  unstable and may deform through crystal
               growth, intake of water of crystallization, or compaction.
                  a)  Prevailing rock types: Nodular and wavy anhydrite, or gypsum interlami-
               nated  with  dolomite.  Such  rock  types  are  commonly  associated  with  redbeds.
                  b)  Color: Highly variable, red, yellow, brown.
                  c)  Grain  type and  depositional  texture:  Very fine  grain  carbonate  sediment;
               gypsum/anhydrite crystals often form a felted mat of tiny lath-shaped crystals or,
               when secondary, are large, bladed, and poikilotopic.
                  d)  Bedding  and  sedimentary  structures:  Laminate,  both  wispy  and  planar
               types,  mud  cracks,  stromatolite  and  spongiostrome  structure,  gypsum  rosettes
               and  selenite  blades  (pseudomorphed  by  anhydrite),  and  syngenetic,  diagenetic,
               and deformational structures such as nodular and chickenwire (flaser) structure,
               enterolithic (contorted) folding. Also diastem surfaces and caliche crusts are com-
               mon.
                  e)  Terrigenous  clastics: May be very common, redbeds and windblown sedi-
               ment.
                  f)  Biota: Almost  no indigenous  fauna  except  for  blue-green  algal  stromato-
               lites, brine shrimp.
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