Page 139 - Carbonate Platforms Facies, Sequences, and Evolution
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DOMING
S 3c
CARIXIAN (EARLY PLIENSBACHIAN)
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5
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10 km
Bathonian (D) and the late Callovian to the beginning of the late Oxfordian (C). 1 =
Q-$-
Valvigneres
0 Villeneuve de Berg
Bourg
penecontemporaneous erosion, 2 = 'Terres Noires' (black shales): late Callovian and early Oxfordian, 3 =
St Andeol
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Fig. 19. Simplified isopach maps and palaeostructural interpretation for the Rhaetian (B), the Carixian (A), the late
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escarpment and
gaps related to non dep o sition or/and
