Grenville orogenic belt

E223835

The Grenville orogenic belt is a vast, ancient mountain-building region in eastern North America and beyond, formed over a billion years ago and representing one of the major Precambrian collisional events in Earth’s history.

All labels observed (2)

Label Occurrences
Grenville basement 1
Grenville orogenic belt canonical 1

How this entity was disambiguated

Statements (51)

Predicate Object
instanceOf Precambrian orogen
geologic province
orogenic belt
ageDescription over one billion years old
approximateAgeInYears 1000000000
associatedWith Rodinia
continent North America
exposedIn Llano uplift
New Jersey
New York
Ontario
Quebec
linked to: Quebec, Canada

Texas
extendsInto Canada
Greenland
Mexico
Scandinavia
South America
United States
western Africa
formedBy continental collision
plate convergence
forms southeastern margin of the Canadian Shield
geologicAge Mesoproterozoic
Neoproterozoic
linked to: Neoproterozoic Era
knownFor deep crustal exposures
high‑grade metamorphism
large‑scale crustal thickening
lithology gneiss
granite
granulite
high‑grade metamorphic rocks
locatedIn eastern North America
maximumAgeMa 1300
metamorphicGrade amphibolite facies
granulite facies
minimumAgeMa 900
namedAfter Grenville Province
orogenicCycle Grenville orogeny
partOf Canadian Shield
Laurentian craton
represents assembly of the supercontinent Rodinia
major Precambrian collisional event
researchField Precambrian geology
structural geology
tectonics
significance key to understanding Proterozoic plate tectonics
records late Precambrian continental assembly
tectonicSetting collisional orogen
timeSpanEndMa 900
timeSpanStartMa 1300

How these facts were elicited

Referenced by (2)

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

Rodinia assemblyLinkedTo Grenville orogenic belt
subject linked to: supercontinent Rodinia
Carolina Slate Belt overlies Grenville basement
linked to: Grenville orogenic belt