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The Quaternary of the Great Hungarian Plain in Loess and the Quaternary: Chinese and Hungarian case studies.
  • The Quaternary of the Great Hungarian Plain in Loess and the Quaternary: Chinese and Hungarian case studies.
  • 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
Neogene-Quaternary geomorphological surfaces in the Hungarian mountains 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.
The Neogene red clays of the Carpathian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • The Neogene red clays of the Carpathian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Opinions differ as to whether the true red clays mostly deposited on Upper Pannonian lacustrine sediments are dated as Pliocene or early Quaternary. Biostratigraphic and lithostratigraphic data show that these non-rewashed residual deposits of red
Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Problems of the Neogene and Quaternary in the Carpathian Basin.
  • A volume for the 8th Congress of the Regional Committee on Mediterranean Neogene stratigraphy, Budapest, September 1985. The study of the conditions and rate of deposition of the several thousand metres of Neogene and Quaternary sediments
A study on the lower boundary of Quaternary in North China. Stratigraphic significance of the Matuyama/Gauss boundary in Loess and the Quaternary: Chinese and Hungarian case studies.
  • A study on the lower boundary of Quaternary in North China. Stratigraphic significance of the Matuyama/Gauss boundary in Loess and the Quaternary: Chinese and Hungarian case studies.
Soil moisture investigations on the loess-covered slopes of the Tokaj area in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Soil moisture investigations on the loess-covered slopes of the Tokaj area in Loess and the Quaternary: Chinese and Hungarian case studies.
Analysis of clay minerals in Hungarian loesses on the basis of the clay mineral map of soils in Hungary in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Analysis of clay minerals in Hungarian loesses on the basis of the clay mineral map of soils in Hungary in Loess and the Quaternary: Chinese and Hungarian case studies.
On the correlation of Eurasian terrestrial stratigraphy in Late Cenozoic times in Loess and the Quaternary: Chinese and Hungarian case studies.
  • On the correlation of Eurasian terrestrial stratigraphy in Late Cenozoic times in Loess and the Quaternary: Chinese and Hungarian case studies.
On understanding the range and stratigraphic position of the Pannonian in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • On understanding the range and stratigraphic position of the Pannonian in Problems of the Neogene and Quaternary in the Carpathian Basin.
A new lithological evaluation and typology of loess exposures in Transdanubia and on the Danube-Tisza Interfluve in Loess and the Quaternary: Chinese and Hungarian case studies.
  • A new lithological evaluation and typology of loess exposures in Transdanubia and on the Danube-Tisza Interfluve in Loess and the Quaternary: Chinese and Hungarian case studies.
Problems of the granulometry of loess in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Problems of the granulometry of loess in Loess and the Quaternary: Chinese and Hungarian case studies.
On the mineralogical and petrological properties of the younger loess in Hungary in Loess and the Quaternary: Chinese and Hungarian case studies.
  • On the mineralogical and petrological properties of the younger loess in Hungary in Loess and the Quaternary: Chinese and Hungarian case studies.
Geochemical characteristics of loess in Luochuan section, Shanxi province in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Geochemical characteristics of loess in Luochuan section, Shanxi province in Loess and the Quaternary: Chinese and Hungarian case studies.
Chronostratigraphy of Hungarian loesses and the underlying subareal formation in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Chronostratigraphy of Hungarian loesses and the underlying subareal formation in Loess and the Quaternary: Chinese and Hungarian case studies.
Limnic and terrestrial sedimentation and the N/Q boundary in the Pannonian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Limnic and terrestrial sedimentation and the N/Q boundary in the Pannonian basin in Problems of the Neogene and Quaternary in the Carpathian Basin.
Tying the basalts from the Transdanubian Central Mountains (Hungary) to the standard polarity time scale in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Tying the basalts from the Transdanubian Central Mountains (Hungary) to the standard polarity time scale in Problems of the Neogene and Quaternary in the Carpathian Basin.
Sketch of the biochronology of the Late Cenozoic in Central Europe in Problems of the Neogene and Quaternary in the Carpathian Basin.
  • Sketch of the biochronology of the Late Cenozoic in Central Europe in Problems of the Neogene and Quaternary in the Carpathian Basin.
Mineralogical observations on the Paks-Dunakomlod loess plateau in Loess and the Quaternary: Chinese and Hungarian case studies.
  • Mineralogical observations on the Paks-Dunakomlod loess plateau in Loess and the Quaternary: Chinese and Hungarian case studies.
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 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 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.