Page 19 - Carbonate Platforms Facies, Sequences, and Evolution
P. 19

basin
                                                              b a s_i n
                        I==
                   �
                   shoal
                         I·  tidal
                                                                                                              we
                              internal
                                                              we
                         flat
                                                                                                              stern
                   complex
                              la�oon
                                                              ste rn
          Massiccio platform in Tuscany.
                                                                                                               margin
                                                              margin
                                                                                                                     CEROIDE
                    �
                         �
                        �
                                                                   MASSIC CIO
                    .
                               open
                   b  astn
                             laQOOn
                        complex
                                                                                                                     LIME
                               {massive
                             bedded
                         sabkha  {subtidal
                                                              pI  all o rm
                        tidal  fl at
                   carbonate
                                                                                                               pI  a  If  ar m
                    { siliciclastic
                                                                                                                     STONE
                                                                   LIMESTONE
                                                              interior
                                                                                                               interi or
                                                                                                                     -LOWER
                                                                   -LOWER
                        breccias
                                                                                         '
                                                                                          '
                                                                                                                     CA
                                                              eastern
                                                                                                                                Carbonate deposition during early rifting,  Italy
                                                                                             '
                                                                                              '
                        v
                        '*
                              0
                    (L)
                          �@
                                                              ma r�in
                              ooids
                                                                   JURASSIC
                          skeletal
                                                                                                                     MBRIA N
                        buildups
                                                                                                               eastern  margin
                                                  u
                                                 u;
                                                   u
                                                    0
                                                "'
                    intraclasts
                                               ::!'
                                                <(
                                                                                                         Middle
                                                                                         400
                                                                           mO
                                                                                  200
                                                                                                      Toyonian
                                                                                                Bo tomion
                                            Raethian
                                                                                                  U.Botomian
                                                  Hettangian
                                                         Sin emurion
            Fig.  5.  Vertical and lateral facies distribution across Lower Cambrian Ceroide platform in Sardinia and Lower Jurassic
                                                                                                         Cambrian
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