Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 14. 1989. (Budapest, 1989)

Devecser (Dv-4) (Figs 3 and 6) These subsidence curves show strong similarity to those of Sv-1; the difference is that in Devecser the sea-floor has reached the 40 m and 100 m "marker"-depths somewhat earlier, and that the accumulated sediment is much thicker. The subsidence history, however, is almost identical: slow and gradual, acceleration can not be pointed out (at least up to the end of the Millecaput Zone). • I II I Fig. 4 subsidence diagram of the section Cr-2. a= sea-floor curve; b= basement curve. For other symbols see Fig. m I Fig. 5 Subsidence diagram of the section Sv-1. Legend: see in Fig. 3 and 4