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Soja-Decke
- Origin of the Name
- Rank
- nappe
- In short
-
The Soja Nappe is a small tectonic unit of the Eastern Lepontic (Ticino Culmination) located between the overlying frontal part of Adula Nappe and the underlying Simano Nappe. To the north, it extends into the Garzott Slices located in the core of the Lunschania Antiform and surrounded by the Piz Terri-Lunschania Nappe. It includes a polycyclic crystalline basement covered by Permian to Jurassic sediments.
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Garzott-Schuppen
- Name Origin
-
Garzott (TI), Lago di Luzzone
- Rank
- tectonic slice
- Status
- valid
- In short
-
The Garzott Slices are considered as a northern extension of the Soja Nappe in the core of the Lunschania Antiform, where they are surrounded by the Piz Terri-Lunschania Nappe. Due to this structural position, Galster et al. (2012) attached the Garzott Slices to the Piz Terri-Lunschania Nappe, but the facies analogies bring them closer to the Soja Nappe (Vögeli et al. 2013).
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Breccia di Garzott
- Name Origin
-
Garzott (TI), Lago di Luzzone
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
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Gneiss di Luzzone
- Name Origin
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
- In short
-
Paragneiss de la zone Piz-Terri-Lunschania: métagrès arkosique et micaschiste verdâtre, avec des intercalations conglomératiques. Unité caractérisée par de fréquentes taches brunes (ankérite), avec également de minces intercalations dolomitiques dans la partie supérieure.
- Age
- Permian
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«Soja-Trias»
- Rank
- lithostratigraphic unit
- Status
- informal term
- In short
-
Dolomitische Abfolge, mit wenigen geringmächtigen Kalklagen, im Dach der Soja-Decke.
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«Soja-Verrucano»
- Rank
- lithostratigraphic unit
- Status
- incorrect name (though informally used)
- In short
-
Gneiss phengitique résultant du métamorphisme d'un grès arkosique avec quelques intercalations conglomératiques.
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Gneiss della Val Soja
- Origin of the Name
- Rank
- lithostratigraphic unit
- Status
- incorrect name (though informally used)
- In short
-
Antico gneiss policiclico nel nucleo della falda della Val Soja: gneiss chiaro a due miche, a grana minuta fino a media, fortemente scistosa.
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