Page 10 - Carbonate Platforms Facies, Sequences, and Evolution
P. 10

© 1990 The International Association of Sedimentologists  ISBN: 978-0-632-02758-3  James Lee Wilson, Paul D. Crevello, J. Rick Sarg, J. Fred Read  9   *  Deceased.   arid   suggests  the shifting  of the continental plates  from   continental break-up connected with the opening of   quences   Bernoulli   opening   phases   quences   The sedimentary evolution of early Mesozoic se­  and then other pelagic  deposits (Fig.  2).   after drowning was buried by red, nodular limestones   platform   depositional   ized  by sequences  which show a  similar




                          of
                        of
                                              Cambrian
                      et  al.,
                                              of
                                                                                   with
                        Tethys
                                     developed
                          continental
                                       evolution.
                      1979).
                            in  Tuscany has
                   of  Sardinia  are
                                     on
                                                                                   limestones.
                          rifting
                                                               whereas
       Carbonate Platforms: Facies, Sequences and Evolution   Edited by Maurice E. Tucker,
                        (Bernoulli
                                       In  both
                   related
                                              southwestern
                        &
                   to
                                     siliciclastic
                                       cases,
                            been  related
                                                                                   Persistence
                          associated
                            to
                                              Sarqinia
                                                                                   of
                        Jenkins,
                                                                   The  subsequent
                                     deposits
                                              and
                          with
                                                               the  latter  evolved
                   early  stages
                      The  Lower  Palaeozoic  se­
                                       a  carbonate
                        1974;
                                     and
                                              the
                   of
                          the
                            the  early
                                                                                                             COCOZZA*
                                                                   evolution
                                                                                   shallow-water
                                                                                                             and
                              1
                   2
                                                               into  an  open
                                                                                                             A.
                                                                                                          University of  Siena,
                            bonate
             to
                        drowned
                                                               ocean.
                                                                                   deposition
             humid
                        under
                                 demonstrate that:
                            platforms
                        a
                                                                                                             GANDIN
                            of
                                            in  Sardinia  gave  way
                                                                                   documents
             tropical
                                                                                   a
             areas
                            Sardinia
                                       folding (Vai &  Cocozza,  1986).
             as
                                         that  resulted  in  pull-a-part  basins
                                                                                   continuous
                            and
                                                               Climatic  changes  occurred
                                                                       Nodular  lime­
                                                               during
                                                                                   balance
                                                                   of  the  basins  reflects  the  different  geodynamic
                        synsedimentary  tectonic
                                            to  oblique  transform
                                                                                                          Via delle  Cerchia 3, 53100 Siena,  Italy
                            Tuscany
                      related to early stages of intra-cratonic rifting;
           divergent movements during continental rifting.
                                                                                                                      the Cambrian of Sardinia and the
                                     The aim of this paper is to compare the sedimen­
                              the Lower Palaeozoic and  Lower Mesozoic car­
                   the climatic change from arid to humid conditions
                        regime
             a  consequence  of
                 recorded within the platform stage of both sequences
                            were
                                            rifting
                                         and  local  gentle
                                   tological characters of the two sequences in order to
                                              the Iapetus Ocean. However, this extensional phase
                          tilted, isolated platforms, established, developed and
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