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  • The Neogene red clays of the Carpathian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Neogene-Quaternary geomorphological surfaces in the Hungarian mountains in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Problems of the Neogene and Quaternary in the Carpathian Basin.
  • The absolute chronology of the Plio-Pleistocene alluvial sequence overlying the pediment of the Matra Mountains in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • The economic geological importance of the lignite at the foreland of the Northern Hungarian Uplands in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • The Great Hungarian Plain is the largest sedimentary basin of Europe filled with great thicknesses of Neogene sediments. The complex mapping of deposits showed that during the Quaternary the maximum degree of subsidence was 700 m and in the lowlands