The origin of the sedimentary filling of the Graupensandrinne (South German
Molasse-Basin) has recently become focus of a scientific discussion. BUCHN
ER (1998) postulates a fluvial genesis whereas REICHENBACHER et al. (1998)
assume an estuary. A detailed sedimentological facies analysis done at seve
ral outcrops reveals evidences for tidal influence.
A reconstruction of the 3-D bedforms was attempted using GPR (Ground-Penetr
ating Radar). This reveals a structural inventory characteristic for tidal
sand-waves.