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A sand dune intercalated by soil horizons was investigated using luminescence and radiocarbon dating methods, to determine the time of aeolian activity and soil formation in the north-eastern part of the Gödöllő Hills in Hungary. Optically stimulated luminescence (OSL) dating and Infrared stimulated luminescence (IRSL) dating of sand sized (100–200µm) grains of quartz and feldspar, respectively, were...
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