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In: Geografický časopis, vol. 53, no. 2
Ladislav Dzurovčin

Morfoštruktúry Polonín a ich postavenie v morfoštruktúrnom pláne Východných Karpát

Detaily:

Rok, strany: 2001, 127 - 146
Kľúčové slová:
relief of fold structures, planated surfaces, valley network, Poloniny Mts., Eastern Carpathians

O článku:

The Poloniny Mts. are situated in the NE of Slovakia. They form an independent geomorphological unit in the framework of high Flysch mountain ranges. They are built by claystone and limestone rocks of the Dukla unit. Morphostructural building of the territory was analyzed by means of satellite images and confronted with the results of field mapping. Single morphostructures of the studied territory represent brachysynclines and brachyanticlines with partial application of fault tectonics. These are considerably destroyed and today represent the passive structures exhumed in the relief-forming stage of the neotectonic phase. The relief reflects the geological structure where the individual erosional forms are linked to lower geomorphologic resistance or to faults. Remains of planated surfaces, which survive in top parts of the individual massifs suggest planation of the original folded mountain range. Stages of gradual uplifting and erosional division of the territory followed the denudation period of the neotectonic stage.

Ako citovať:

ISO 690:
Dzurovčin, L. 2001. Morfoštruktúry Polonín a ich postavenie v morfoštruktúrnom pláne Východných Karpát. In Geografický časopis, vol. 53, no.2, pp. 127-146. ISSN 0016-7193.

APA:
Dzurovčin, L. (2001). Morfoštruktúry Polonín a ich postavenie v morfoštruktúrnom pláne Východných Karpát. Geografický časopis, 53(2), 127-146. ISSN 0016-7193.