Dr. Nagy I. Zoltán szerk.: Fragmenta Mineralogica Et Palaentologica 2. 1970-71. (Budapest, 1971)

depth of deposition: 40 to 100 m. At the end of the Late Eocene the Globigerinae make their appearance. J. The line Andornaktálya-Kács. Highest rate of sinking. Continental deposits are missing, even the"shallow-water deposits are poorly developed (noth sampled). Upper Eocene is represented by pelagic deposits of the Cylindroclavulina cylindrica Zone; there is no evidence as to the presence of the Globigerina gortanii - Globorotalia /T./ centralis Zone, which would be en equivalent of the Bryozoan Marl. CORRELATION OF SOME UPPfRST EOCENE-MIDDLE OLIGOCENE STRATIGRAPHIC SEQUENCES IN HUNGARY AND IN EUROPE H OF Mm, K. mi M4JiOM,l 1986 PRESENT WORK SAMUEL - SALA J BLOW t9S9 BExeesEN im BUDA /OFEHi BUDA-BÜKK Mrs BUOAPEST BÜKK MTS mi SLOVAKIA N-EUROPE 1 CLAY OF fC/SCíLL GL OBI BE PIMA >> <> ft IKLÍINZBLUR RUPELIAN »CLAY OF KISCELL " SELL II- PSEUDOHASTIGERINA •*> "t> Üj TEGEL} LEVELS 1-4 BARBADOS HSIS P 19_ t-. Ci 1 SIKATtS WITH PISH - JCALí urn %, . TAR

01 AN' ^fy-^tAC/ES OF JARD' i i AÏ & t 5 * §/ Ni -H 5 i s § § fr. Ül S; o» to i- !>, 1 ^ Ob r5 / ZONE OF SMALL £ / 61 OBIGE RIMAS *"> / M-l ^3 S; o» to i- !>, 1 ^ Ob rI EOCENE - OLIGOCENE TRANS1 X to i- !>, 1 ^ Ob rIzOMB Of CrUMÙROCLAVU-^^' ILMA CYLINDRICA %LimeCr i „S0V/ND •1 ih <"» •'.-) 3e BRYOZOA MARL [BRYÙZOA MARL" marls wth liihci frammvm, dry ozoa, AummutltS, Aster,getmo.MAeiino and tin iinttitol sêdimtnts N 5 5 Ç) Í1 55 > i "*i •S S *> OL OBIGE NINA 6- GORTANII eiOBOROTALIA TTl CENTRALIS MARL ' P17 P17 Table III.j Comparât

ion of several Upper Eocene and Middle 011gocene profiles from Hungary and other European countries. Ill, táblázati Néhány felső eocén-középső oligocén szerelvény összehasonlítása Magyarországon és Európában,