Acasta Gneiss Complex

E803743

The Acasta Gneiss Complex is one of the oldest known rock formations on Earth, consisting of highly metamorphosed ancient continental crust located in the Canadian Shield of Northwest Territories, Canada.

Try in SPARQL Jump to: Statements Referenced by

Statements (47)

Predicate Object
instanceOf Archean terrane
gneiss complex
rock formation
ageRange approximately 4.03–3.6 billion years
composition amphibole
biotite
feldspar
quartz
contains Eoarchean rocks
Neoarchean rocks
containsRockWithAge 4.0 billion years
4.02 billion years
4.03 billion years
continent North America
country Canada
crustType continental crust
datingMethod U-Pb zircon geochronology
discoveredBy geologists of the Geological Survey of Canada
discoveryPeriod 1980s
geologicalAge Archean
hostRockType tonalite–trondhjemite–granodiorite suite
knownFor being among the oldest known rocks on Earth
preserving early continental crust
lithology granite gneiss
granodioritic gneiss
orthogneiss
paragneiss
tonalitic gneiss
locatedIn Canadian Shield NERFINISHED
Northwest Territories NERFINISHED
locatedNear Acasta River NERFINISHED
locatedNorthwestOf Yellowknife NERFINISHED
locatedOn Slave craton NERFINISHED
metamorphicFacies amphibolite to granulite facies
metamorphicGrade high-grade metamorphism
namedAfter Acasta River NERFINISHED
oldestDatedRockAge about 4.03 billion years
partOf Slave Province NERFINISHED
region northwestern Canadian Shield
researchField Precambrian geology
geochronology
petrology
significance constrains early Earth crust formation
provides evidence for early plate processes
surfaceExposure small outcrops
tectonicSetting ancient continental crust
usedAs reference locality for Earth’s oldest crust

Referenced by (1)

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

Eoarchean Era hasRockRecord Acasta Gneiss Complex