Mots-clés
Carpates Cycle géomorphologique Erosion différentielle Hongrie Hydrosystème Hydrothermal Karst Karstification Lac Mouvement vertical Paléogéographie Pénéplaine Recharge naturelle Sédiment lacustre Carpathian Mountains Differential erosion Geomorphic cycle Hungary Hydrosystem Hydrothermal Karst Karstification Lacustrine sediment Lake Natural recharge Palaeogeography Peneplain Vertical movementMulti-phase geomorphological evolution of the Keszthely Mountains (SW-Transdanubia) and karstic recharge of the Hévíz lake
Geomorphology and changing environments in Central Europe
Auteurs :CSILLAG, G.
NÁDOR, A.
BREMER, H.
Description :
AA. provide an overview of the geomorphic evolution from tropical peneplanation in the Cretaceous and of the stages of karstification beginning with the Oligocene. The main goal of investigation was to understand the role of the Keszthely Mountains in the hydrogeological system of the Hévíz lake. The paleogeographical reconstruction was based on large-scale geological models. A special attention was paid to the geomorphological control on sedimentation and karstification. The consequences of differential erosion in the Miocene are also discussed. The age of the hydrothermal activity in the Keszthely Mountains is still debated.
Type de document :
Congrès
Source :
European Regional Geomorphological Conference, International Association of Geomorphologists, Hongrie, 1996-04-09, Zeitschrift für Geomorphologie. Supplementband, issn : 0044-2798, 1997, n°. 110, p. 15-26, Collation : Illustration, Références bibliographiques : 20 ref.
Date :
1997
Editeur :
Pays édition : Allemagne, Berlin ; Stuttgart, Borntraeger
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)