Schmiedwirt-Member

Torna a falda di ricoprimento del Lechtal

Rappresentazione e statuto

Rango
Membro litostratigrafico (Sotto-formazione)
Uso
Unità non usata
Status
termine locale (informale)

Nomenclatura

Deutsch
Schmiedwirt-Member
English
Schmiedwirt Member
Varianti storiche

Adneter Kalke s.str. (Tollmann 1976a), Schmiedwirt-Member (Böhm et al. 1995)

Gerarchia e successione

Unità sovrastante

Età

Geomorfologia
  • Sinemuriano
Età alla base
  • Sinemuriano

Referenze

Definizione
Böhm Florian, Dommergues Jean-Louis, Meister Christian (1995) : Breccias of the Adnet Formation: indicators of a Mid-Liassic tectonic event in the Northern Calcareous Alps (Salzburg/Austria). Geol. Rundschau 84, 272-286

p.273: The Schmiedwirt Member is characterized by medium- to thin-bedded intraclastic wackestones with ostracodes, sponge spicules and crinodal debris, partly showing a nodular fabric. It is best exposed in the Schmiedwirt quarry (Fig. 2). Only its lower part is preserved at Adnet and Breitenberg. It is of Sinemurian age and constitutes the major part of the 'Adneter Kalke s. str.' of Tollmann (1976a).

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