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In the sequence of the continental margin of Tethys in the Carpathian region within the age range from Vendian to Miocene occur several organic rich formations. Geochemical investigations of rocks allowed distinguishing the potential petroleum source rocks, to trace their geochemical and thermal evolution from sedimentogenesis to catagenesis and to estimate the depths range of possible hydrocarbon generation. Key words: organic matter, genetic type of kerogen, oil generation potential, thermaldoi:10.30836/igs.2522-9753.2008.152429 fatcat:b5lskzn6u5g4lhaljoz5kmplkm