Gföhl Unit
E884890
The Gföhl Unit is a high-grade metamorphic rock complex within the Bohemian Massif, notable for its granulites and migmatites formed under extreme pressure and temperature conditions.
Statements (30)
| Predicate | Object |
|---|---|
| instanceOf |
geological unit
ⓘ
metamorphic rock complex ⓘ |
| characterizedBy |
extreme pressure conditions
ⓘ
extreme temperature conditions ⓘ |
| contains |
felsic granulites
ⓘ
mafic granulites ⓘ migmatitic gneiss ⓘ orthogneiss ⓘ paragneiss ⓘ |
| formedDuring |
Paleozoic
NERFINISHED
ⓘ
Variscan metamorphic event NERFINISHED ⓘ |
| hasLithology |
granulite
ⓘ
migmatite ⓘ |
| hasMetamorphicFacies |
amphibolite facies
ⓘ
granulite facies ⓘ |
| hasPetrologicalFeature |
high-pressure mineral assemblages
ⓘ
migmatization ⓘ partial melting ⓘ |
| locatedIn |
Austria
ⓘ
Central Europe ⓘ Czech Republic NERFINISHED ⓘ |
| metamorphicGrade | high-grade metamorphism ⓘ |
| overlies |
Moldanubian basement
NERFINISHED
ⓘ
Monotonous Unit ⓘ |
| partOf |
Bohemian Massif
NERFINISHED
ⓘ
Moldanubian Zone NERFINISHED ⓘ |
| researchedFor |
Variscan tectonometamorphic evolution
ⓘ
crustal thickening processes ⓘ exhumation of deep crustal rocks ⓘ |
| tectonicSetting | Variscan orogen NERFINISHED ⓘ |
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.