Ghölzwald-Member
Back to Muot-da-Rubi-FormationRepresentation and status
- Color CMYK
- (0%,8%,51%,4%)
- Color RGB
- R: 245 G: 225 B: 120
- Rank
- lithostratigraphic Member (Subformation)
- Validity
- Unit is in Use
- Status
- valid formal name
Nomenclature
- Deutsch
- Ghölzwald-Member
- Français
- Membre du Ghölzwald
- Italiano
- Membro del Ghölzwald
- English
- Ghölzwald Member
- Origin of the Name
- Historical Variants
- Ghölzwaldschichten (Frey 1965), Ghölzwald Member (Menkveld-Gfeller et al. 2016)
Description
- Description
- Das Ghölzwald-Member besteht aus einem glimmerreichen, sandigen Kalk und einem kalkigen, glimmerreichen Sandstein.
- Thickness
- Ein paar Meter (Menkveld-Gfeller et al. 2016).
Hierarchy and sequence
- Upper boundary
- Tektonischer Kontakt
- Lower boundary
- Stad-Formation
Age
- Age at top
-
- Priabonian
- Age at base
-
- Priabonian
Geography
- Geographical extent
- Zentralschweiz (Linthtal).
- Type locality
-
-
Ghölzwald (GL), nördlich Stelli
Site particularities- typische Fazies
- (2717430 / 1194250)
- Frey 1965
-
Ghölzwald (GL), nördlich Stelli
Palaenography and tectonic
-
- Tertiary
- Tectonic unit (resp. main category)
- Kind of protolith
-
- sedimentary
- Metamorphism
- non metamorphic
References
- Definition
-
2016) :
Lithostratigraphic units of the Helvetic Palaeogene: review, new definition, new classification. Swiss J. Geosc. 109/2, 171-199
(
p.188: The Ghölzwald Member was described by Frey (1965; ‘‘Ghölzwald-Schichten’’), the type locality is at Ghölzwald, Stelli (2717.430/1194.250). Lithology: Above the slaty marlstone of the Stad Formation follow few dm- thick beds of micaceous sandy limestone and calcareous, mica-rich sandstone. Occasionally, a weak gradation can be observed. The overall thickness of the sandy part sums up to only a few meters. Overlying strata: tectonic boundary; underlying strata: Stad Formation. Biostratigraphy: Priabonian, Larger foraminifera. Current geographical extent: Central Switzerland: Linth valley. Tectonic unit: Central Switzerland: Lower Helvetic.