Die tektonische bedeutung von terrassendeformationen

Rok, strany: 1985, 252 - 267

In the light of the results of geomorphological Investigations of the Danube terraces the author has concluded that height differences of the terraces were caused by young crustal movements. In the Pleistocene the mountain range rose by 200 – 250 m compared with the present curve of the Danube. On the other hand the central part of the Little Plain subsided by about 200 m. The Quaternary subsidence in the middle Danube – Tisza region reached 150 – 200 m and in the Southern part it amounted to 250 – 450 m. The comparison of Danube terraces with fluvial deposits allows to estimate the trend, range and time of tectonic movements.

ISO 690:

Pécsi, M. 1985. Die tektonische bedeutung von terrassendeformationen. In Geografický časopis, vol. 37, no.2-3, pp. 252-267. 0016-7193.

APA:

Pécsi, M. (1985). Die tektonische bedeutung von terrassendeformationen. Geografický časopis, 37(2-3), 252-267. 0016-7193.

Vydavateľ: Geografický ústav SAV/Institute of Geography of the Slovak Academy of Sciences