Kaapvaal Craton

E162085

The Kaapvaal Craton is one of Earth’s oldest and most stable pieces of continental crust, located in southern Africa and renowned for hosting some of the world’s richest gold deposits.

All labels observed (4)

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf Archean craton ⓘ
craton ⓘ
geological province ⓘ
age Archean ⓘ
associatedWith early Earth tectonics studies ⓘ
formation of early continental crust ⓘ
comparedWith Pilbara Craton ⓘ
contains Barberton Greenstone Belt ⓘ
Bushveld Igneous Complex ⓘ
Vredefort impact structure basement ⓘ
linked to: Vredefort Dome

Witwatersrand Basin ⓘ
linked to: Witwatersrand
continent Africa ⓘ
country Botswana ⓘ
Eswatini ⓘ
South Africa ⓘ
Zimbabwe ⓘ
crustalThickness about 35–40 km ⓘ
formsPairedCratonWith Pilbara Craton ⓘ
geologicalEra Archean Eon ⓘ
hasEconomicImportance chromite mining ⓘ
diamond mining ⓘ
gold mining ⓘ
platinum mining ⓘ
hasFeature thick lithospheric mantle root ⓘ
hasOldestRocksDated older than 3.5 billion years ⓘ
hostsDepositType layered mafic-ultramafic intrusion deposits ⓘ
orogenic gold deposits ⓘ
paleoplacer gold deposits ⓘ
hypothesizedToHaveBeenPartOf Vaalbara supercraton ⓘ
knownFor hosting diamond-bearing kimberlites ⓘ
hosting platinum-group metal deposits ⓘ
hosting rich gold deposits ⓘ
stability of continental crust ⓘ
lithology granite-greenstone terranes ⓘ
high-grade gneiss terrains ⓘ
lithosphericThickness up to about 200–250 km ⓘ
locatedIn southern Africa ⓘ
linked to: Southern Africa
maximumAge about 3.6 billion years ⓘ
minimumAge about 2.5 billion years ⓘ
overlainBy Transvaal Supergroup ⓘ
Ventersdorp Supergroup ⓘ
Witwatersrand Supergroup ⓘ
partOf African Plate ⓘ
Precambrian basement of southern Africa ⓘ
researchField Precambrian geology ⓘ
economic geology ⓘ
geochronology ⓘ
tectonicSetting stable continental interior ⓘ

How these facts were elicited

Referenced by (28)

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

Witwatersrand → partOf → Kaapvaal Craton ⓘ
Rodinia → contains → Kalahari craton (in many models) ⓘ
subject linked to: supercontinent Rodinia
linked to: Kaapvaal Craton
Barberton Makhonjwa Mountains → partOf → Kaapvaal Craton ⓘ
Kalahari Craton → contains → Kaapvaal Craton ⓘ
Mesoarchean Era → hasRepresentativeCratons → Kaapvaal Craton ⓘ
Pilbara Craton → comparedWith → Kaapvaal Craton ⓘ
Pilanesberg Alkaline Ring Complex → partOf → Kaapvaal Craton ⓘ
Mozambique Belt → boundedBy → Kaapvaal Craton ⓘ
subject linked to: Mozambique belt
Transvaal karst region → locatedOn → Kaapvaal Craton ⓘ
subject linked to: transvaal karst region
Bushveld Igneous Complex → hostCraton → Kaapvaal Craton ⓘ
Barberton Greenstone Belt → partOf → Kaapvaal Craton ⓘ
Witwatersrand Supergroup → locatedIn → Kaapvaal Craton ⓘ
Witwatersrand Supergroup → partOf → Kaapvaal Craton ⓘ
Transvaal Supergroup → locatedIn → Kaapvaal Craton ⓘ
Vaalbara supercraton → formedFrom → Kaapvaal craton ⓘ
linked to: Kaapvaal Craton
Vaalbara supercraton → contains → Kaapvaal craton ⓘ
linked to: Kaapvaal Craton
Vaalbara supercraton → namedAfter → Kaapvaal craton ⓘ
linked to: Kaapvaal Craton
Ventersdorp Supergroup → locatedOnCraton → Kaapvaal Craton ⓘ
Ventersdorp Supergroup → region → Kaapvaal Craton ⓘ
Bushveld region → overlies → Kaapvaal Craton ⓘ
Rehoboth Subprovince → isSeparatedFrom → Kaapvaal Craton ⓘ
Kimberley kimberlite fields → partOf → Kaapvaal Craton ⓘ
Zimbabwe Craton → analogOf → Kaapvaal Craton ⓘ
Zimbabwe Craton → formsPartOf → Zimbabwe–Kaapvaal cratonic region ⓘ
linked to: Kaapvaal Craton
Limpopo Belt → separates → Kaapvaal Craton ⓘ
Limpopo Belt → formsCollisionZoneBetween → Kaapvaal Craton ⓘ
Limpopo Belt → boundedBy → Kaapvaal Craton ⓘ