Olenek Uplift

E781046

The Olenek Uplift is a major geological highland within the Siberian Craton, exposing some of the region’s oldest and most stable Precambrian rocks.

All labels observed (1)

Label Occurrences
Olenek Uplift canonical 1

How this entity was disambiguated

Statements (29)

Predicate Object
instanceOf cratonic highland
geological uplift
tectonic high
characterizedBy ancient crystalline rocks
structural stability
contains oldest rocks of the Siberian Craton region
country Russia
erosionalState deeply eroded basement exposure
exposes Precambrian basement rocks
formsPartOf Siberian Shield NERFINISHED
geologicalAge Precambrian NERFINISHED
hasGeologicalSignificance provides exposure of Archean and Proterozoic rocks
records early continental crust evolution
hasResearchInterest Precambrian stratigraphy
Precambrian tectonics
crustal evolution of the Siberian Craton
hasTectonicHistory long-term stability since Precambrian time
isOneOf major geological highlands of the Siberian Craton
lithologyIncludes gneiss
granite
metamorphic rocks
locatedIn Sakha Republic NERFINISHED
northeastern Siberia
namedAfter Olenyok River NERFINISHED
overlainBy younger sedimentary cover in surrounding areas
partOf Siberian Craton NERFINISHED
structuralType basement high
tectonicSetting stable craton interior
usedFor regional geological correlation in Siberia

How these facts were elicited

Referenced by (1)

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

Siberian Craton hasCoreRegion Olenek Uplift