Abstract: Abstract The approximately 50-m thick loess/palaeosol sequence at Paks brickyard (Hungary) was deposited largely during the Brunhes normal polarity chron and its magnetic properties resemble those of similar sections in Europe, Central Asia and China. In order to get information on the grain size dependence of some of the magnetic parameters, two loess and two palaeosol samples were separated into a number of grain size fractions. The separation method employs consecutive sedimentation and centrifugation steps performed on bulk samples suspende...
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