Page 132 - Carbonate Platforms Facies, Sequences, and Evolution

SE
BASIN

Aubenas, E =
limestones, 8 =
NW
SAINT-AMBROIX
Pliensbachian), Do =
pelagic limestones, 5 =
LV
SW
Isocrinus coquinas, 12 =
highly condensed levels, 16 =
Escrinet Pass, LV =
PAIOLIVE AXIS
•�31 �2 JI:+J31!!!d41
d. LATE BAJOCIAN
R
f. LATE BATHONIAN
e. EARLY BATHONIAN
neptunian dykes.
Les Vans, P =
turbidites and slumps, 13 =
AUBENAS
UZER
SWELL
Fig. lOa, the tilt block is situated westward (Luol High =
Domerian (late Pliensbachian). 1 =
open-sea deposits (Hettangian), 6 =
Privas, R =
/
A
coarse terrigenous clastics and conglomerate, 9 =
b. LATE SINEMURIAN. EARLY CARIXIAN
erosion, 14 =
/
a. LATE HETTANGIAN. EARLY SINEMURIAN
v
SUB-BASIN
lineament TL).
Rosieres, V =
NE
!sJi' / !6 i;"1:j):7 J00°o0 Ja
alternating marls, 2 =
J-z.cJ12JUU J13J�J14�1sE@16
MV
E
Late Triassic and Jurassic platforms, France
oolitic iron ore, 10 =
WSW
SWELL
ESCRINET
AU
sediment winnowing, 15 =
Vesseaux, Ca =
limestones, 3 =
p
protected deposits (mottled limestones), 7 =
PRIVAS
/ SUB-BASIN
�9 �10 [£}11
sandy
Carixian, (early
Main localities are shown on Fig. 9: A =
ENE
ferruginous stromatolite, 11 =
marly limestones, 4 =
non-depositional gap and
Fig. 10. Palaeobathymetric and palaeostructural evolution of the Ardeche from the Hettangian to the late Bathonian. In
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