Page 281 - Carbonate Facies in Geologic History

tv 0- 00 :::0 C1> !l, >-l .... C1> ::l 0- m ~ ::l 0- tt! ~ '" 5· o .g o ~. '" 5· r' a C1> '-< s:: .... ~ m '" n· '"Ii ~ 0;. '"

section

of line
OXFORDIAN and for

MTS,

JURA

MUMIENKALK SWISS

2km Fig.IX-3. Cross section of Oxfordian strata in Swiss Jura Mountains. For legend see Fig.III-l Fig. IX-4. Shows silty and onkoidallime mudstone facies oflagoons passing through oolitic grainstone with patch reefs of coral across a coral bank to thin-bedded brown bioclastic wackestone and argillaceous beds of the basin. Prograd

(1970)

~ -. ~
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