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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.
(supprimer)
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).