Körnung und Schwermineralbestand als Kriterien für eine Deckschicht in der Umgebung von Seefeld und Leutasch (Tirol)

Ernst Schönhals & Thomas J. Poetsch
With the help of the grain size distribution and the heavy mineral analysis it was proved that the soil lying on top of the limestone gravels dit not develop there but was formed by an eolian deposit (cover layer) instead. It is therefore a profile consisting of two layers.