The Freikofel Formation consists of three well-bedded facies listed in order of decreasing abundance. Facies A: medium dark gray, medium to thick bedded, moderately sorted lithoclastic rudstone (subordinately floatstone) sometimes showing fining upward grading; matrix consists of grainstone (subordinately wacke-/packstone); Facies B: medium dark gray, thin to medium bedded grainstone and subordinate packstone locally showing fining upward grading; planar and subordinate cross lamination is present; Facies C: very thin to thin bedded, moderate pink to gray mud-/wackestone.

Pondrelli, M., Pas, D., Spalletta, C., Schönlaub, H., Farabegoli, E., Corradini, C., et al. (2015). Freikofel Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 121-124.

Freikofel Formation

SPALLETTA, CLAUDIA;FARABEGOLI, ENZO;PERRI, MARIA CRISTINA;
2015

Abstract

The Freikofel Formation consists of three well-bedded facies listed in order of decreasing abundance. Facies A: medium dark gray, medium to thick bedded, moderately sorted lithoclastic rudstone (subordinately floatstone) sometimes showing fining upward grading; matrix consists of grainstone (subordinately wacke-/packstone); Facies B: medium dark gray, thin to medium bedded grainstone and subordinate packstone locally showing fining upward grading; planar and subordinate cross lamination is present; Facies C: very thin to thin bedded, moderate pink to gray mud-/wackestone.
2015
Pondrelli, M., Pas, D., Spalletta, C., Schönlaub, H., Farabegoli, E., Corradini, C., et al. (2015). Freikofel Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 121-124.
Pondrelli, M.; Pas, D.; Spalletta, C.; Schönlaub, H.P.; Farabegoli, E.; Corradini, C.; Suttner, T.J.; Corriga, M.G.; Perri, M.C.; Da Silva, A.C.; Simo...espandi
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/545590
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