Berlingen-Member
Rappresentazione e statuto
- Colore CMYK
- (0%,24%,35%,4%)
- Colore RGB
- R: 245 G: 185 B: 160
- Rango
- Membro litostratigrafico (Sotto-formazione)
- Uso
- Unità in uso.
- Status
- termine formale valido
Nomenclatura
- Deutsch
- Berlingen-Member
- Français
- Membre de Berlingen
- Italiano
- Membro di Berlingen
- English
- Berlingen Member
- Origine del nome
-
Tiefbohrung bei Berlingen (TG)
- Varianti storiche
-
Berlingen Member (Jordan et al. 2016)
Descrizione
- Descrizione
-
Grobkörnige alluviale und fluviale Sandsteine von Vindelizianischem Ursprung. (Jordan et al. 2015)
- Potenza
- bis zu 5 m (Jordan et al. 2016)
Componenti
- fedspato
Gerarchia e successione
- Unità di rango superiore
- Limite superiore
-
Wiedereinsetzen von buntem Mergel über Sandstein.
- Limite inferiore
-
Einsetzen von Sandstein über buntem Mergel.
Età
- Geomorfologia
-
- Carnico
- Età alla base
-
- Carnico
Geografia
- Estensione geografica
- Nordöstliche Schweiz
- Regione-tipo
- Seerücken-Gebiet (TG/SH/ZH)
Paleogeografia e tettonica
-
- Trias (Jura)
- Paleogeografia
- Rheingraben
- Termini generici
-
-
Jura
:
Juragebirge
-
Jura
:
- Tipo di origine
-
- sedimentaria
- Condizioni di formazione
-
sandige Randfazies mit Vindelizianischem Ursprung.
- Metamorfismo
- non metamorfo
Referenze
- Definizione
-
(2016) :
The middle to late Triassic Bänkerjoch and Klettgau formations of northern Switzerland. Swiss J. Geosc. 109/2, 257-284
In the wells Berlingen and Herdern (both in Canton Thurgau),a coarse-grained sandstone with calcitic matrix is found at the level where the Gansingen Member is expected (sandy layers of «Bunte Mergel (mit Sandlagen)» by Büchi et al. 1965). The sandstone can clearly be distinguished from the fine-grained Ergolz Member sandstone. These layers are significantly older than the Seebi Member, to which they show some similarities. Bläsi (1995) correlated these layers with the «Kieselsandstein» of southern Germany (now Hassberge Formation, e.g. Etzold and Schweizer 2005).
Definition: Middle-grained to coarse-grained, poorly sorted sandstone with quartz, feldspar and rocky fragments of the surrounding members. The matrix contains quartz cement, sulphate or clay in alternation with layers of clayey sandstone and claystone with dolomite nodules.