Une tectonique synsedimentaire originale du Miocene moyen des environs de Budapest, marquer de l'extension du bassin pannonien.Middle Miocene synsedimentary tectonic structures near Budapest: evidence for extensional process within the Pannonian Basin.

Synsedimentary tectonics that created remarkable patterns of NE-SW tension gashes have affected the Badenian strata near Budapest. Ridges of oomicrite bind these fissures and correspond to an early cementation that occurred contemporaneously with sedimentation. The creation of these tension gashes is connected with the opening of the Pannonian Basin and, in detail, is interpreted as the earlier stage of an extensional process that leads to the development of larger normal faults.