Vaalbara supercraton

E636175

Vaalbara supercraton is a proposed early Archean supercontinent thought to have formed from some of Earth’s oldest cratons, including the Kaapvaal and Pilbara cratons.

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Observed surface forms (1)

Statements (44)

Predicate Object
instanceOf hypothetical geological entity
supercontinent
associatedWith early Archean sedimentary basins
early continental crust growth
early plate tectonics
breakupProcess Archean rifting and subduction
contains Kaapvaal craton NERFINISHED
Pilbara craton NERFINISHED
country Earth NERFINISHED
disputedBy some geologists
evidenceType geochronological data
paleomagnetic data
stratigraphic correlation
structural geology
followedBy Kenorland supercontinent NERFINISHED
Superia supercraton NERFINISHED
formedFrom Kaapvaal craton NERFINISHED
Pilbara craton NERFINISHED
hasAge more than 3.0 billion years
hasMaximumAge about 2.7 billion years
hasMinimumAge about 3.6 billion years
hasRockRecord banded iron formations
greenstone belts
komatiites
hasSignificance constrains models of early Earth thermal evolution
represents one of Earth’s earliest large continental assemblies
hasUncertainty exact configuration of cratons
exact time of assembly
exact time of breakup
locatedInPeriod Archean eon NERFINISHED
Mesoarchean era
Paleoarchean era NERFINISHED
namedAfter Kaapvaal craton NERFINISHED
Pilbara craton NERFINISHED
nameEtymology portmanteau of Kaapvaal and Pilbara
partOf early Earth tectonic history
possibleLocation present-day Western Australia
present-day southern Africa
precededBy Hadean proto-continents NERFINISHED
researchField Precambrian geology
paleomagnetism
tectonics of early Earth
status proposed
supportedBy paleomagnetic reconstructions of Kaapvaal and Pilbara

Referenced by (2)

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

Kaapvaal Craton hypothesizedToHaveBeenPartOf Vaalbara supercraton
Pilbara Craton formsWith Vaalbara supercraton
this entity surface form: Pilbara–Kaapvaal supercraton (hypothesized)