>
Az üledékképzodés szakaszossaga az Alfod negyedidoszaki rétegeiben. (Periodicity of sedimentation in the Quaternary layers of the Great Hungarian Plain)
(supprimer)
In the sedimentation cycles coarse and fine deposits grade into each other with no sharp boundaries. Periods of several years and those of several ten thousands of years are also observed. Combined with malacological, palynological, climatological