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(Upper Miocene, Lake Pannon, cement marls, lithology, stratigraphy, paleomagnetism, Beočin, Fruška Gora)
parameters), which originates from neoformed magnetite.Key words: Upper Miocene, Lake Pannon, cement marls, lithology, stratigraphy, paleomagnetism,Beočin, Fruška Gora.Апстракт: У раду су приказане главне литолошке, структурне

measured section of borehole IB-9 and ofthe exposed deposits in the bordering areas indicatedheterogeneous lithology of the Sarmatian (Fig. 4).Lithologically, it consists of laminated marl, sandymarl, banded silty marl and

angle between 5° and8°. The Upper Pontian strata consist entirely of sandysediments, distinctly different in lithology from theolder Pannonian marls. Pontian deposits begin with alayer of ferruginous silty sandstone, abounding