The Hoher Trieb Formation consists of five well-bedded facies listed below: Facies A: medium dark gray very thick-bedded rudstone and floatstone; matrix consists mainly of grainstone; silicified corals are common among the clasts; Facies B: medium dark gray thin to thick-bedded pack-/grainstone locally showing evidence of tractive structures; Facies C: medium dark gray thin to medium-bedded wackestone; Facies D: black thin to medium-bedded laminated cherts; cherts are also locally present in nodules mainly within facies C; Facies E: black very thin to thin-bedded laminated shales.

Pondrelli, M., Schönlaub, H., Corradini, C., Spalletta, C., Suttner, T., Kido, E., et al. (2015). Hoher Trieb Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 125-128.

Hoher Trieb Formation

SPALLETTA, CLAUDIA;PERRI, MARIA CRISTINA;
2015

Abstract

The Hoher Trieb Formation consists of five well-bedded facies listed below: Facies A: medium dark gray very thick-bedded rudstone and floatstone; matrix consists mainly of grainstone; silicified corals are common among the clasts; Facies B: medium dark gray thin to thick-bedded pack-/grainstone locally showing evidence of tractive structures; Facies C: medium dark gray thin to medium-bedded wackestone; Facies D: black thin to medium-bedded laminated cherts; cherts are also locally present in nodules mainly within facies C; Facies E: black very thin to thin-bedded laminated shales.
2015
Pondrelli, M., Schönlaub, H., Corradini, C., Spalletta, C., Suttner, T., Kido, E., et al. (2015). Hoher Trieb Formation. ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT, 69, 125-128.
Pondrelli, M.; Schönlaub, H.P.; Corradini, C.; Spalletta, C.; Suttner, T.J.; Kido, E.; Perri, M.C.; Simonetto, L.; Corriga, M.G.; Mossoni, A.; Pohler,...espandi
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/545591
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