Mennyiben pontosíthatja a georadaros vizsgálat a homokterületek geomorfológiai kutatásának eredményeit? : Komplex tanulmány egy belső-somogyi homokbuckán = Can georadar surveying contribute to clarifying aeolian research results? : Complex study on a sand dune in Inner Somogy, Hungary

Györgyövics, Katalin and Katona, Orsolya (2016) Mennyiben pontosíthatja a georadaros vizsgálat a homokterületek geomorfológiai kutatásának eredményeit? : Komplex tanulmány egy belső-somogyi homokbuckán = Can georadar surveying contribute to clarifying aeolian research results? : Complex study on a sand dune in Inner Somogy, Hungary. A KAPOSVÁRI RIPPL-RÓNAI MÚZEUM KÖZLEMÉNYEI (4). pp. 5-12. ISSN 2064-1966 (nyomtatott); 2631-0376 (elektronikus)

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Abstract

A complex geomorphological research was carried out on an aeolian sand dune in Inner Somogy, Hungary. Sedimentological analysis showed three layers of sediment composed of sand with differing characteristics (Györgyövics et al., 2014) which suggested at least 3 aeolian phases in the region. OSL dating of samples from the same boreholes confirmed these periods and determined that sand was deposited during the Late Glacial, the Dryases and Boreal phase (Kiss et al. 2012). However, carrying out a GPR survey revealedmuch more detailed structure of the particular dune. Comparing research results and applying GPR profiling in the early stages of geomorphological investigation could help choosing the OSL sampling points and depths resulting in a more precise study.

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