Page 131 - Carbonate Platforms Facies, Sequences, and Evolution

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Rousse
Profiles: X=
Les Eynesses
CNC
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to middle Bathonian beds, 4 =
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-
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Map: X= metamorphic schists, 1 =
·
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Le Moignard
CCB
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l Forheran
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FCB
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Ucel Variegated Formation (Carnian-Norian?), FCB =
Elmi
FBU
t-,;;;;;�j
r
MC
E£EJ
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=
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EARLY
and FF'). The principal measured sections are located on the map drawn on Fig. 6.
mud-cracks filled by sandstones. Adapted from Colongo et al. (1979) and Elmi (1984).
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.
.
· .· . �� . _:___ �
LS
-�
·
late Bathonian (west) or early Callovian (east) to late Jurassic:
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.
. -=-:=----�---==-:.._ ·
.
Croix Blanche Formation (Rhaetian), CCB =
HETTANGIAN 1
· 'Fcs �'--=-=--=
X
-=--
WE1
ESE
Complete
Carbonate de Base (earliest Hettangian), CNC = Calcaires noduleux cendres Formation (early Hettangian), FS = giant
dynamic style is obvious between the Carnian-Norian (normal faults: FE and FF) and the Rhaetian (antithetic faults: FE'
pre-Rhaetian Triassic, 2 = Rhaetian and early Hettangian, 3 = reduced Domerian
Fig. 9. Palinspastic reconstruction of the latest Triassic and early Jurassic terranes along the Orcieres Fault. The change in
metamorphic schists, LS = Lower sandstones (Ladinian), MC = middle carbonates (early Carnian), FBU