Page 262 - Carbonate Facies in Geologic History
P. 262
trl :>< i Dl 8., tt! § ~ '" § 0- ::0 <1> <1> (;i> ~ \0
knoll. and kn:lbs
,HI
... "., fl als
Vlianow w .. t ... ban_ ... mud ..,.". Wllh ""o,-/Sypralidal mud IIaIS _ -;--;=:--
~ Fig. VIII-20. Paleogeographical interpretation of depositional environments during the Late Rhaetian. Note that all reefy shelf margins and bioherms
--..... " . _
time$lone
Dach$teln
RoelO-liu~ Reel are composed of superimposed reef knolls and knobs. From Zankl (1971, Fig. 3)
bed$
I<i:)$SM Hauptdolomt