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(Article of periodic en Hongrois - 1980)

Document title

A Balaton kornyéki neotektonika. (Neotectonics in the Lake Balaton region)

Authors(s) and Affiliation(s)

MIKE K. ;

Abstract

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 are genetically related with flexing stresses observable along the strike of the Highland Range. (CK).

Source

Article of periodic

published at : Foldrajzi Kozlemenyek Budapest

Editor :

Millesime : 1980, vol. 28, no3 [pp. 185-204]

Bibliographic references : 87 réf.

Language

Hongrois

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