Uffiern-Diorit

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Representation and status

Index
delta-U
Color CMYK
(0%,48%,56%,6%)
Color RGB
R: 240 G: 125 B: 105
Rank
lithostratigraphic Formation
Validity
Unit is in Use
Status
informal term
Status discussion

Nomenclature

Deutsch
Uffiern-Diorit
Français
Diorite du Val Uffiern
Italiano
Diorite della Val Uffiern
English
Uffiern Diorite
Origin of the Name

Umgebung der Fassungsanlage Bucca di Uffiern (GR), im wetlischen Val Uffiern (Seitental der Val Cristallina)

Historical Variants

Diorit des Val Ufirn (Grubenmann 1892), Diorit der Val Ufiern = Ufierndiorit (Winterhalter 1930), Ufiern-Diorit = Ufirn Diorit (Rutsch et al. 1966), Ufiern-Sädelhorndiorit, Uffien diorite (Mercolli et al. 1994), Uffiern-Diorit (Vögeli et al. 2013)

Hierarchy and sequence

Age

Age at top
  • Early Permian
Age at base
  • Late Carboniferous (= Pennsylvanian)

Geography

Geographical extent
Östliches Gotthardmassiv.
Type locality
  • Bucca digl Uffiern (GR)
    Site particularities
    • typische Fazies
    • historische Fundstelle
    Site accessibility
    • Strassenanschnitt / Bahnanschnitt
    Coordinates
    • (2709500 / 1161200)
    Note
    • Heim 1891, Vögeli et al. 2013
Point of interest
  • Tuors (GR)
    Site particularities
    • typische Fazies
    Site accessibility
    • Grat
    Coordinates
    • (2709080 / 1160200)
    Note
    • Vögeli et al. 2013

Palaenography and tectonic

Tectonic unit (resp. main category)
Kind of protolith
  • plutonic
Metamorphism
monocyclic

References

Definition
Heim Albert (1891) : Geologie der Hochalpen zwischen Reuss und Rhein. Mit einem Anhang von Petrogr. Beiträgen von C. Schmidt. Beitr. Geol. Karte Schweiz 25, 605 Seiten

R. Müller und E. Niggli in: Rutsch et al. 1966: UFIERN-DIORIT (= Ufirn Diorit = Uffiern-Diorit) (Jungpaläozoikum ; Gotthardmassiv): Alb. Heim (1891) in: Geologie der Hochalpen zwischen Reuss und Rhein. Beitr. geol. Karte Schweiz. 25: 226. Kleiner Dioritstock (0.5 auf 1 km) des östlichen Gotthardmassivs nach R. U. Winterhalter (1930) innerhalb des südlichen Cristallina-Granodiorits (>>>) liegend. Nach der Val Ufiern benannt (= Val Uffiern der LK 256, 711000/161300, Seitental der Val Cristallina). Mittelkörniger, massiger quarzführender Hornblende-Biotit-Diorit, mit normaldioritischem Chemismus. Literatur: Alb. Heim (1891), C. Schmidt (1891: 25), U. Grubenmann (1892: 139-142), R. U. Winterhalter (1930: 77-82).

Definition
Berger Alfons, Mercolli Ivan, Herwegh Marco, Gnos Edwin (2017) : Geological Map of the Aar Massif, Tavetsch and Gotthard Nappes. Geological Special Map 1:100'000, Explanatory Notes 129

p.72: p.72: The Uffiern Diorite, the Cristallina Granodiorite and the Medel Granite constitute a single coherent plutonic complex towards the eastern end of the Gotthard Nappe. The Medel Granite is coarse-grained and locally porphyric, while the Cristallina Granodiorite is more fine-grained and equigranular. MERZ (1989) described the petrographic and structural characteristic of both units. VÖGELI et al.(2013) described the small occurrence of the Uffiern Diorite. The Medel Granite envelops the northern and the western part of the complex, whereas the Cristallina Granodiorite occupies the centre and the southern part. The roughly north–south oriented western intrusive contact of the Medel Granite perpendicularly crosscuts the steeply east–west oriented structures of the polycyclic metamorphic basement (Ausserbinn-Piz Cavel Zone) as well as the pre- to early Variscan metasedimentary and volcaniclastic sequences of the Val Rondadura Group. This is one of the important observations that allowed the reconstruction of the pre-Alpine evolution of the Gotthard Nappe (see MERCOLLI et al.1994 and references therein).

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