Hoher Trieb Formation

Autor: 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, S. M. L., Hüneke, H
Přispěvatelé: 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, S. M.L., Hüneke, H, Schönlaub, H. P., Suttner, T. J., Perri, M. C., Corriga, M. G., Pohler, S. M. L.
Jazyk: angličtina
Rok vydání: 2015
Předmět:
Popis: 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.
Databáze: OpenAIRE