Incision of a river curvature due to exhumed Miocene volcanic landforms: Danube Bend, Hungary

International Journal of Earth Sciences

Volumn 95, Issue 5, 2006, Pages 929-944

  Karatson D ^a   Nemeth K ^b,f   Szekely B ^a,c   Ruszkiczay Rudiger Zs ^a,d   Pecskay Z ^e  

^a EÖTVÖS LORÁND UNIVERSITY   (Hungary)

^b GEOLOGICAL INSTITUTE OF HUNGARY   (Hungary)

^c UNIVERSITY OF TÜBINGEN   (Germany)

^d Netherlands Research Centre for Integrated Solid Earth Science ISES   (Netherlands)

^e INSTITUTE OF EXPERIMENTAL MEDICINE   (Hungary)

^f MASSEY UNIVERSITY   (New Zealand)

Author keywords

Differential uplift; Horseshoe shaped caldera; Miocene volcanism; Pannonian basin; River incision

Indexed keywords

CALDERA; EROSION RATE; EXHUMATION; GEOMORPHOLOGY; LAVA DOME; MIOCENE; PALEOGEOGRAPHY; PLEISTOCENE; VOLCANIC LANDFORM; VOLCANISM; VOLCANOLOGY;

CENTRAL EUROPE; DANUBE BEND; EURASIA; EUROPE; HUNGARY; PANNONIAN BASIN;

EID: 33748174540     PISSN: 14373254     EISSN: 14373262     Source Type: Journal    
DOI: 10.1007/s00531-006-0075-9     Document Type: Article

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