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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.
  • Bassin Pannonien ; Géochronologie ; Géographie physique ; Hongrie ; Néogène ; Quaternaire ; Stratigraphie ; Sédiment lacustre ; Sédimentologie
  • The change from limnic to terrestrial sedimentation is regarded as a marker of the N/Q boundary in the Carpathian basin. It is roughly synchronous with the Matuyama-Gauss paleomagnetic reversal (million years). The boundary is easy to trace
  • in mountains, but more difficult to define in basins where oscillations of water level took place. DLO).
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.
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.