Controls on facies mosaics of carbonate platforms: a case study from the Oxfordian of the Swiss Jura - Perspectives in Carbonate Geology - page 200

Pertuis Savagnières Gorges de Court Hautes-Roches Vorbourg

7 k 2 k 9 k 1 k

4 m

10

3 m

10

9

3 m

? ?

30
m

30

8

7 20

?

m M W P G

20

6

? ?

20

5

Ox 6

20

Facies
limestone with quartz
marls
peloids
oncoids
ooids
lithoclasts
brachiopods
echinoderms
benthic foraminifera
corals
bivalves
gastropods
serpulids
charophytes
plant fragments

Texture
marls
mudstone
wackestone
packstone
grainstone
floatstone / rudstone
boundstone

4

m
M
W
P
G
F/R
B

3

10

10

2

10

Sedimentary Structures
birdseyes
bioturbation
cross-stratification
microbial mat

1

10

m M W P G F/R B

Sequence- and Cyclostratigraphy

100-kyr sequence boundaries
400-kyr sequence boundaries
400-kyr maximum floodings
sequence boundary according
to Hardenbol et al . ( 1998)

m M W P G F/R B

m M W P G

Ox 6

m M W P G B

Fig. 6. Correlation of 100- and 400-kyr sequences between the sections studied. Only major facies elements and sedimentary structures are indicated in the lithological
columns. For discussion refer to text.