Age-depth models and dust-mass accumulation rates for loess-palaeosol sequences from the Carpathian Basin
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Figure 1 represents the Bacon.r age-depth models for the: a) Irig b) Nosak c) Stari Slankamen and d) Crvenka loess-palaeosol sequences while figure 2 shows the corresponding dust-mass accumulation rates (minimum, maximum, mean and median values) calculated according to the modeling results for the same sites. Appendix A contains the modeled ages for the Irig, Nosak Stari Slankamen and Crvenka loess-palaeosol sequences.
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Zoran Peric
