East European Craton

E410800

The East European Craton is an ancient, stable part of the continental lithosphere underlying much of Eastern Europe, forming the geological core of regions such as Russia, Ukraine, and the Baltic states.

All labels observed (3)

Label Occurrences
East European Craton canonical 2
Baltic Shield basement 1
Baltic craton 1

How this entity was disambiguated

Statements (44)

Predicate Object
instanceOf craton
geological province
boundedBy Caledonian orogenic belt
linked to: British Caledonides

Ural Orogen
linked to: Ural Mountains

Variscan orogenic belt
characterizedBy ancient continental lithosphere
tectonic stability
thick continental crust
continentPart Eurasia
formedDuring Precambrian
hasAlternativeName Baltic Craton
East European Shield (in shield areas)
hasCoreRegion Baltic Shield
linked to: Baltica

Ukrainian Shield
Volgo-Uralia
linked to: Volga-Ural region

Voronezh Massif
hasEconomicImportance hydrocarbon basins
mineral resources
hasGeologicalAge Archean
Paleoproterozoic
hasProperty forms geological core of Eastern Europe
one of the largest Precambrian cratons
hasRockType gneiss
granite
high-grade metamorphic rocks
hasTectonicFeature platform areas
shield areas
isPartOf Laurentia–Baltica paleocontinent system
locatedIn Eastern Europe
overlainBy Phanerozoic sedimentary cover
partOf Baltica
East European Platform
studiedInDiscipline geology
geophysics
tectonics
underlies Belarus
Estonia
Latvia
Lithuania
Russia
Ukraine
parts of Finland
parts of Poland
parts of Sweden

How these facts were elicited

Referenced by (4)

Full triples — surface form annotated when it differs from this entity's canonical label.

Smolensk–Moscow Upland geologicalProvince East European Craton
Baltica hasAlternativeName Baltic craton
linked to: East European Craton
Ukrainian Shield partOf East European Craton
Grenville orogeny preservedIn Baltic Shield basement
linked to: East European Craton