Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 15. 1992. (Budapest, 1992)

with pure limestone layers, the bedding surfaces are even or nodular in various degree; the fauna is relatively poor. At about the middle of the section the limestone is overlain by almost pure siliceous deposits: this 70 cm thick, thinly bedded interval is made up of spiculitic chert. Above a 40 cm thick fossiliferous limestone intercalation the spiculitic chert becomes predominant again. It is very thinly layered, the bedding surfaces are undulating and 1-2 cm thick clay interbeds are frequent in the upper part. The spiculitic chert is terminated abruptly and the Text-fig. 2. - Detailed lithological column of the temporary exposure at the Szobrosbánya locality with symbols of the most important fossils found. 1: limestone; 2: siliceous and cherry limestone; 3: spiculitic chert ; 4: coarse nodular limestone, clay interbeds. B: belemnites; C: Chlamys; E: Entolium; G: Gryphaea; H: Homoeorhynchia; L: Liospiriferina; P: Pseudopecten