-
Falda della Cima Lunga
- Origin of the Name
- Rank
- nappe
- Status
- valid
- In short
-
The Cima Lunga Nappe is a tectonic unit of the Eastern Lepontic (Ticino Culmination). It is made up of paragneisses, orthogneisses, sheets of marble and calcschist as well as lenses of mafic and ultramafic rocks that locally have an incoherent character. Eclogitic mineral assemblages are widespread in the mafic and ultramafic rocks. Sheath folds around the disrupted competent mafic and ultramafic lenses suggest intense shearing within a shear zone at the base of the Maggia Nappe. According to most authors, the Cima Lunga Nappe is connected in the east, to the Adula Nappe in the lower Valle Mesolcina.
-
Gneiss di Rognoi
- Origin of the Name
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
- In short
-
Gneiss leucocratico a due miche con enclavi di anfibolite e nidi di biotite della Falda della Cima-Lunga.
-
Gneiss di Vacarisc
- Origin of the Name
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
- Age
- Permian
- In short
-
Ortogneiss leucocratico a due miche, p.p. occhiadino della Falda della Cima-Lunga.
-
Gneiss di Vogorno
- Origin of the Name
- Rank
- tectonically bounded lithostratigraphic unit
- Status
- informal term
- In short
-
Gneiss oligoclasico chiaro a due miche, con microclino, a grana fine, con livelli mesocratici, della falda della Cima Lunga.
-
Eclogite dell'Alpe Arami
- Origin of the Name
- Rank
- lithostratigraphic unit
- Status
- informal term
- In short
-
Eklogitisierter Peridotit der Cima-Lunga-Decke.
- Nomenclatorial Remarks
-
peridotiti granatifere dell'Alpe Arami
-
Peridotite della Cima di Gagnone
- Origin of the Name
- Rank
- lithostratigraphic unit
- Status
- local name (informal)
- Age
- Early Cambrian
- In short
-
Eklogisierter Granat-Lherzolit der Cima-Lunga-Decke.