Page 270 - Carbonate Platforms Facies, Sequences, and Evolution
P. 270

FACIES  1   FAC IES  3   FACIES  4   FACIES  5o  5b   FAC IES  6   FACIES  8   FACIE S  9
 LI GHT  TO  DAR K.   DARK MICROBIOCLAST IC   COARSE  LITHOCL�STIC-  M!CR! rE  RliD :ST  KNGLLS  YI ITH   loou I IC
 LAM INATE  TO   AND  PELAG IC  MICRITS  BIOCLASTIC,   CREAM� SHELL�  TH IC K-REDDED   GRAIN STONE   MICRI TE�  THJN
 HOMOGENEOUS,   TH ICK  TO  TH IN   BOULDERS  IMBEDDED   LIMFSTONE .   MED IUM  BEDS.  MI NOR  LANE  BANK,   v  <  .
 PELAG IC  MICRI TE,   RHYTHM IC  BEDD ING.   IN  MICRITE,   CYC LES  OF  MILIOLID   0
 FI NELY  CALCARENITIC   DARK  CHERT  NODULE S.   CRA I NSTONE;  B I OTLRBA TI'I   "'
 IN  PLACES.   SLUMP  STRUCTURES .   WACKESTONE  TO  LAMINA  TIT   v
 OVERLAPPING   FAC IES   � �ESTRAL  Ml CR ITE   �
           LCt11TE  CRUSTS
 PLANKTON IC   PLANKTON IC   11 JXED  BIOTA,   CAPR IN IDS,   CAPR IN IDS   CAPR INID  OEBR IS   RESTR ICTED  BIOTA,
 MI CROFOSS ILS;   MI CROFOSS ILS;   MA INLY  DEBR IS  FRO�\   RAD IOLIT!DS,   DOM INATE ,   �ill  (RAo. )   ALGAL
 COLON IAL  CORALS  W.\LCli_S.LI\  ON
 AMMONI TES,   ,;�JMON ITES,   UPSLOPE,   STRCt1ATOPOROI OS,   MOUND  TOPS,   tiERtJ.E   BI OSTROMES  OF   MI LIOLID
 ENCRUST! NG  ALGAE,   I-
 GLOB I GER IN I OS,   GLOB !GE RINIDS,   (SA)   (HONPRQJlQ!ilA   PARKE8..L8  (STROM. )   B.Eill!l..E.l  &�.
 PHOL A9  (BORING   AT  TOP .   0
 TINTINNIDS.   TltHINNIDS,   CLAMS  ,   tiE.lli.�   S.O.LUIQPQR.I\  (RED  ALGA)  GRYPHAEA  WHEN  MARLY,   ""   0  "'
 0J CTYOCONUS   ( LARGE  FORAMS),  Coo 1 A.CEAN   0
 Mi CROPELOIOS.   0ASYCLADACEANS,   c=; ·
 (BENTHON IC   M I L1 OLIOS,
    DASYCLADACEAN
 FORAM) ,   Dl.il..l.,   8
    �bhi���DS, (LARGE
          111 LIOLIOS.   &
 \   \  \   Outer  kn olls  Inner  knolls   I  I   '  '  '   Zl   0
 \   \   2 o� l   I  '   0  �0   I   "'   /'- �I   �  (';;'
 \   \   slope   \  I   I  (  li1"  '\\\{�"'   A   A   �  <">
       .
 \   \   �\I 1/'l'-  ,, ,  /   0   •   00  �  :-<5-  W I   --� ·
 ��� 0
 \   \  \   'fJ   Interre ef  sands
 \   \   (1   Sa li nity   in crease   �I  �
 \   \   0  0.       � I   §'
 ..   /   '   /   ..   \   �   "<?  To me bra  Lst   El Abra  Lim estone   "'  >  z
 _.J.-...._,
 ...
 - ..  /   ..  : :  /  -  ....   /   0  •   -.L�----&/   w
 BATHYA L-TAMAU LI PAS  TO E  OF  SLOPE  FOREREEF   SHELF  MARGIN  KNO LLS   INNER  BANK   I- z
 FACIES   TAMA ULIPAS   CLASTICS   AND  PATCH  REEFS   w  I-
 many  km  wi de   2km  wide   2km  wide   few  km  wide   lOOkm  across   X  w
 Fig.  12. Idealized middle Cretaceous facies across rimmed platform in central Mexico.  From Wilson  (1975,  figs X
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