Page 201 - Carbonate Platforms Facies, Sequences, and Evolution
P. 201
line shown in (c).
receipt by the authors. (b)
section. (c) Migrated 48-fold
some interpretative lines were
24-fold dynamite line. Note that
drawn on this section prior to its
related buildup on the northwest
side of the basin. (a) Unmigrated
Interpretation of line shown in (a)
Ramalhal part of the salt structure
vibroseis line. (d) Interpretation of
Fig. 14. Seismic sections across the
showing mounded clinoforms at the
top of the Upper Jurassic carbonate
NNW
NNW
r---
1km
two
two
Ramal hal
!al
time
sees
time
sees
way
way
sw
SW
t\
OXFORDIAN
ti
CARBONATES
Ramalhal
UPPER
Ramalhal#t
# 1
JURASSIC
LOURINHA
Upper Jurassic carbonate buildups,
CARB ONATES
TOJIERA
Portugal
AB1 DIA
-,op
AMARAL "
TOP DAG ORDA
AMARAL
TOP MIDDLE JU RASSIC
0
TOP OAGORDA
LOURI NHA
tkm
-------
anhydrite
SSE
=
NE
SSE
N E
187
M>O-�
0
2
(c)
(d)
two
time
SE!CS
way