Page 205 - Carbonate Platforms Facies, Sequences, and Evolution

Sintra.

This formation
metamorphozed
is
to
Fig. 18. Summary log of
Kimmeridgian-Tithonian
The Ramalhao formation
slates),
dominated
Abano, on the coast southwest of
Sequence exposed north of Praia do
but
by shales
.·
!-.�� 1
II
resedimented
.
.
F=
B
shale
car-
(thermally
thin
below
:::;:
"'
Oi
"'
£
:::;:
E
.§
packs tones
thin-bedded
limestone
supported
supported
breccia
300m
300
thick.
250
200
predominantly
predomi nantly
turbiditic
beds
breccia
clast
matrix
Cl>
c:
:::;:
:::;:
"'
E
Oi
Upper Jurassic carbonate buildups, Portugal
wackestones.
400
350
450 '
�
�
The
and
with
and
• bedded
nodular
thin beds
massive
lime
lime
formation
p =pec kestones
w=wackestones
is
above
packestones
=
wackestones
md =lirne mudstones
500
bedded wac kestones
300m
mudstones
some wac kestones
mudstones
lime mudstones
400 m
bonates occur at the base as thin breccia beds and
191