Page 288 - Carbonate Platforms Facies, Sequences, and Evolution

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Limit
Slump
of
Siliceous
Siliceous
coral
Limestone
Mudstones
Bioturbated
Autochthonous
outcrops
breccias
turbidites
breccias
Scouring -excavation
sandstones
conglomerates
urgonian
surface
and
Somorrostro area, to the northwest of Bilbao.
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A slump bed is seen in the centre of the picture.
LAPATZA
Fig. 19. Talus deposits consisting predominantly of
limestones
siltstones
autochthonous micritic limestones alternating with marls.
F
'
EA
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sedimentary sector).
Aptian-Albian carbonate episode, Spain
Platform sedimentary sectors). The slope apron megabreccias of unit C filled longitudinally (in
'
APIKALE
Fig. 18. Urgonian limestone megabreccias and terrigenous talus deposits from the Ea area (Guernica and Northern
N-S direction) the Ea
Fig. 20. Monotonous black marls with a slump fold 5 m
trough. A-H: sedimentary units. R1 -R5: local sedimentary breaks. After Agirrezabala & Garcia-Mondejar (in press).
thick. Basinal sediments of the Soba area (west of Bilbao
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