Page 264 - Carbonate Facies in Geologic History

tTl >< po 3 '0 (; V> o ....., to po ~ ~ en po ~ 0- ~ (l) (l) i7' N Vl

Merg~
-- Netherlands
- dunkelgrau
- The
- Bottom two sections show color
- Leiden,
e ba n k t~z .T. knollig-- Zunahme des Tonaehaltes Fig.4). Company, and Brill

mass i g~g farblos Farbinillnsitlil From Fabricius (1966, and of author

Zunahme dcrr Tethyan geosyncline. intensity increasing in both directions from reef front and changes in gross rock type and bedding off shelf from well-bedded to massive to bedded and in part nodular in the direction of the basin (Becken-Fazies). Associated with this basinward change in bedding is an increas

K 0 M P LEA northern Illustration with

Iff f f - gebankt .---------------------------------------------------~ base.

Fazies Achlerrifl of wave

t calcllulitischc reflexion and a

Oolith-<;: fazies >- ! grau I Fig. VIII-21. Facies diagram of Late Triassic in suspension

sediment