First application of the 10Be/9Be dating in the Alpine orogenic realm
Relative biochronology validated by absolute 10Be/9Be authigenic ages
Effective application to lacustrine and floodplain samples from outcrops and boreholes
Progradation of deltaic systems across the Danube Basin lasted from 11.0 to 9.4 Ma
Heterochronous onset of alluvial sedimentation from 10.5 to 8.7 Ma in NW-SE direction