Zur Korrelation der Terrassen und Lösse in Österreich

J. Fink
The contributions of the field geologists to the knowledge of the younger pleistocene cover mostly loess-sediments, terraces and moraines; only the two first mentioned sections are dealt with here. In Austria the occurrence of the loess is restricted to the foreland of the Alps and the Vienna basin. This region can be subdivided into three subregions (fig. 1) on the basis of differences in the develoment of fossil soils, intercalated within the loess. An equivalent...