Rae craton

E552522

Rae craton is an ancient, stable block of Earth’s continental crust that forms a major geological core of the Canadian Shield within the North American craton.

All labels observed (1)

Label Occurrences
Rae craton canonical 3

How this entity was disambiguated

Statements (44)

Predicate Object
instanceOf craton
geological province
ageRange greater than 2.5 billion years
associatedOrogeny Taltson–Thelon orogeny
Trans-Hudson orogeny
boundedBy Churchill Province
Hearne craton
Slave craton
characteristic ancient continental crust
forms a major geological core of the Canadian Shield
tectonically stable
country Canada
crustalThickness relatively thick continental crust
economicGeology base metal deposits
diamond-bearing kimberlites
gold deposits
hosts mineral resources
uranium deposits
formedBy accretion of Archean terranes
geologicalAge Archean
Paleoproterozoic
heatFlow low
lithology granitoid plutons
granulite-facies rocks
greenstone belts
high-grade gneiss
metasedimentary rocks
locatedIn North America
Northwest Territories
Nunavut
northern Manitoba
northern Saskatchewan
northwestern Canadian Shield
linked to: Canadian Shield
oldestRocksAge about 3.0–3.2 billion years
overprintedBy Paleoproterozoic orogenesis
partOf Canadian Shield
North American craton
linked to: Laurentian craton
researchField Precambrian geology
craton evolution
significance important for reconstruction of early Proterozoic supercontinents
key to understanding assembly of the Canadian Shield
records early continental crust formation
structuralElement Churchill craton
tectonicSetting interior of North American plate

How these facts were elicited

Referenced by (3)

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

Laurentia includesRegion Rae craton
Laurentian craton hasPart Rae craton