Brunovistulian terrane
E900441
The Brunovistulian terrane is a Precambrian to early Paleozoic crustal block in Central Europe that forms part of the basement underlying the eastern Variscan orogen.
Statements (47)
| Predicate | Object |
|---|---|
| instanceOf |
crustal block
ⓘ
geological unit ⓘ terrane ⓘ |
| associatedWithOrogeny | Variscan orogeny NERFINISHED ⓘ |
| basementFor | eastern Variscan orogen NERFINISHED ⓘ |
| boundedBy |
East European Craton
NERFINISHED
ⓘ
Moldanubian Zone NERFINISHED ⓘ Teplá–Barrandian terrane NERFINISHED ⓘ |
| exposedIn |
Austria
NERFINISHED
ⓘ
Czech Republic NERFINISHED ⓘ Poland NERFINISHED ⓘ Slovakia NERFINISHED ⓘ |
| formsBasementOf |
Moravo-Silesian Zone
NERFINISHED
ⓘ
southern part of the Bohemian Massif ⓘ |
| geologicalAge |
Precambrian
ⓘ
early Paleozoic ⓘ |
| hasCrustalAge |
Cambrian
ⓘ
Neoproterozoic ⓘ Ordovician ⓘ |
| hasCrustalCharacter | peri-Gondwanan microcontinent fragment ⓘ |
| hasDeformationAge | Variscan ⓘ |
| hasEconomicInterest | potential mineral resources ⓘ |
| hasMagmatismAge |
Cambro-Ordovician magmatism
GENERATED
ⓘ
Neoproterozoic magmatism GENERATED ⓘ |
| hasMetamorphicGrade |
low-grade metamorphism in parts
ⓘ
medium-grade metamorphism in parts ⓘ |
| hasProtolithAge |
Paleozoic
GENERATED
ⓘ
Proterozoic GENERATED ⓘ |
| hasStructuralStyle | polyphase deformation ⓘ |
| hasTectonicAffinity | peri-Gondwanan terranes ⓘ |
| isSubunitOf | Bohemian Massif NERFINISHED ⓘ |
| lithologyIncludes |
gneisses
ⓘ
granitoids ⓘ metasedimentary rocks ⓘ metavolcanic rocks ⓘ |
| locatedIn | Central Europe ⓘ |
| namedAfter | Brno and Vistula regions NERFINISHED ⓘ |
| partOf | Central European basement ⓘ |
| relatedTo | Cadomian orogeny NERFINISHED ⓘ |
| researchTopicIn |
Central European geology
ⓘ
Variscan tectonics ⓘ |
| separatedFrom | East European Craton by the Trans-European Suture Zone ⓘ |
| studiedUsing |
geochronology
ⓘ
petrology ⓘ structural geology ⓘ |
| tectonicSetting | accreted to the Variscan orogenic belt ⓘ |
| underlies | eastern Variscan orogen NERFINISHED ⓘ |
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.