Page 140 - Carbonate Platforms Facies, Sequences, and Evolution

N
+
palaeostructural

LATE RIFTING
S 7 pars
S Sa
LATE BATHONIAN
POST-RIFTING
LATE CALLOVIAN to
measured section (selection), 9 =
MIDDLE OXFORDIAN

estimated values, 10 =
0

5
erosion. Adapted from Elmi (1967, 1987) and from Elmi et al. (1984).

fft
10 km
important boreholes, 11 =
o$-
valvigneres
Q Villeneuve de Berg
localities, 12 =

lineaments (explanation of abbreviations and code-numbers given in Fig. 21), 7 = isopach line, 8 =
penecontemporaneous
Fig. 19. (Cont.) zones of rapid thickening, 4 = umbilic and sense of thickening, 5 = major positive or stable axes, 6 = major