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(Article of periodic en Anglais - 2012)

Document title

Ductile and brittle deformations in the Sopron Gneiss Formation (Sopron Mts., W-Hungary) and their implication on the formation of the Pannonian Basin

published at : Geomorphological environments. Research methods on biotic and abiotic anvironments

Authors(s) and Affiliation(s)

BENKÓ Z. (1) ; BUGLEDITS E. (1) ; RÉCSI A. (1) ;
(1) Dep. of Physical Geography, Fac. of Earth Sciences, Univ. of West Hungary, Szombathely, HONGRIE

Abstract

The crystalline complex of the Sopron Mts. at the eastern end of the Austroalpine nappe system and on the western rim of the Pannonian Basin is a key area to investigate the relationship of orogenic and extensional-rift structures that led to the formation of the Pannonian Basin. The AA. focused primarily on the brittle and ductile deformations in 3 selected gneiss outcrops (Nádormagalast, Harka Hill, Kö Hill). Beyond providing evidence for the possible rotation and tilting of the different blocks of the mountains based on the comparison of the structural elements, they paid special attention to the brittle-plastic deformations that may indicate the (re-)activation of Cretaceous thrust faults

Source

Thematical fascicle

published at : Zeitschrift für Geomorphologie / ISSN 0372-8854 / CODEN ZGMPAG

Editor : Gebruder Borntraeger, Stuttgart - ALLEMAGNE (1925)

Millesime : 2012, vol. 56, no 2 [pp. 3-19]

Bibliographic references : 42 ref.

Collation : fig., tabl.

Language

Anglais

INIST-CNRS, Cote INIST : 8829

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1127/0372-8854/2012/S-00082

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2012
Refdoc record number (ud4) : 26722603 : Permanent link - XML version
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