Supplementary material to "First evidence of active transpressive surface faulting at the front of the eastern Southern Alps, northeastern Italy. Insight on the 1511 earthquake seismotectonics"

Abstract

Unit 2: colluvial deposit made of yellowish/brownish sandy silt with sparse cm-size polygenic pebbles and charcoals fragments. Interpretazione stratigrafiche nel unità poligeniche tagliamento Unit 3: colluvial deposit made of brownish massive sandy silt containing cm-size polygenic pebbles (mostly organised in gravel lenses), charcoal fragments and Fe-Mn concretions. Unit 4: alluvial deposit made of clast-supported gravel with brownish silty matrix. Unit 5: colluvial deposit made of massive yellowish-brownish sandy silt containing cm-size polygenic pebbles (mostly organised in gravel lenses), charcoal fragments and Fe-Mn concretions Unit 6: colluvial deposit made of yellowish and locally brownish clayey silt with sparse clasts (10 cm maximum size). The deposit underwent pedogenesis which altered the surface of the clasts and the whole sediment structure, and determined the formation of Fe-Mn concretions. Unit 7: alluvial deposit made of polygenic gravel (cm-size pebbles) laterally grading to clayey silt with sparse pebbles. The pebbles lithology attests that the deposit has been fed by the Tagliamento R. catchment.. Unit 8: bedrock represented by the Savorgnano Flysch (Ypresian, Early Eocene). Table 2: (INNOVA SCARL laboratory). Centro per lo Sviluppo ed il trasferimento dell'Innovazione nel Settore dei Beni culturali e Ambientali-INNOVA Scarl. Via Cairoli 81,