Aspects of Fluvial Sedimentation in the Lower Triassic Buntsandstein of Europe [Paperback]

Prologue.- Spectrum of local sedimentary elements.- Braidplain, floodplain and playa lake, alluvial-fan, aeolian and palaeosol facies composing a diversified lithogenetical sequence in the permian and triassic of South Devon (England).- Gravel bars in braided-river channels of the basal buntsandstein-facies conglomerates in the cuenca province (Southeastern Iberian ranges, Central Spain).- Depositional models of braidplains intertonguing with aeolian dune fields.- Aeolian sedimentation in the middle buntsandstein in the eifel north-south depression zone.- Depositional mechanisms and facies models of intertonguing aeolian environment and fluvial milieu in the middle buntsandstein of the mid-european triassic basin.- Sandy inland braidplain deposition with local aeolian sedimentation in the lower and middle parts of the buntsandstein and sandy coastal braidplain deposition in the topmost zechstein in the sudetes (Lower Silesia, Poland).- Fluvial sedimentary styles and associated depositional environments in the buntsandstein west of river rhine in saar area and pfalz (F.R. Germany) and vosges (France).- Depositional models of braidplains with associated calcrete pedogenesis.- Depositional mechanisms controlling formation of coarse fluvial conglomerates in the lower triassic continental red beds of middle europe.- Sandy braidplain deposition with minor pedogenesis in the labyrinthodontidae beds (middle buntsandstein) of the northeastern holy cross mountains (Poland).- Minor pedogenesis and local aeolian influences in sandy to pebbly braidplain deposits of the solling-folge (upper buntsandstein) in the hessian depression (hessen and lower saxony, F.R. germany).- Depositional models of braidplains without coexisting non-fluvial environments.- Gravelly to sandy braidplain deposition in the czerwona g?ra beds and stryczowice beds (middle buntsandstein) of the northeastern holy cross mountains (poland).- Gravelly to sandy braidplain deposition in the buntsandstein-facies bolãg