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  • The quaternary structural conditions revealed in the neighbourhood of Lake Balaton are the results of kratogenic phases of movement. The folds and on echelon faults formed parallel to the strike of the Transdanubian Central Moutains are due to minor
  • compressions that revived in the period of tectonic relaxation. Perpendicularly to the arcuate on echelon fault lines, tension faults of similarly arcuate strike were formed along which some horizontal displacements also took place. These later phenomena
  • 1980