Witwatersrand Supergroup
E635113
The Witwatersrand Supergroup is a thick sequence of ancient sedimentary rocks in South Africa renowned for hosting some of the world’s largest gold deposits.
Observed surface forms (1)
| Surface form | Occurrences |
|---|---|
| Witwatersrand Basin | 3 |
Statements (45)
| Predicate | Object |
|---|---|
| instanceOf |
geological formation
ⓘ
sedimentary rock sequence ⓘ supergroup ⓘ |
| age |
Mesoarchean
ⓘ
Neoarchean ⓘ |
| contains |
auriferous conglomerate
ⓘ
placer-type gold deposits ⓘ pyrite ⓘ uraninite ⓘ uranium-bearing conglomerate ⓘ |
| country | South Africa ⓘ |
| depositionalEnvironment |
deltaic
ⓘ
fluvial ⓘ shallow marine ⓘ |
| economicImportance |
major source of gold production
ⓘ
major source of uranium production ⓘ |
| geologicalPeriod | Archean ⓘ |
| hasResearchInterest |
Archean sedimentology
ⓘ
early Earth atmosphere ⓘ early Earth hydrosphere ⓘ |
| hostRockFor | Witwatersrand goldfields NERFINISHED ⓘ |
| knownFor |
large gold deposits
ⓘ
uranium deposits ⓘ |
| lithology |
banded iron formation
ⓘ
conglomerate ⓘ quartzite ⓘ sandstone ⓘ shale ⓘ |
| locatedIn |
Kaapvaal Craton
NERFINISHED
ⓘ
Witwatersrand Basin NERFINISHED ⓘ |
| maximumAgeInYears | 3050000000 ⓘ |
| minimumAgeInYears | 2700000000 ⓘ |
| namedAfter | Witwatersrand NERFINISHED ⓘ |
| overlies | Pongola Supergroup NERFINISHED ⓘ |
| partOf | Kaapvaal Craton NERFINISHED ⓘ |
| region |
Free State Province
NERFINISHED
ⓘ
Gauteng Province NERFINISHED ⓘ North West Province NERFINISHED ⓘ |
| stratigraphicUnitOf | Witwatersrand Basin NERFINISHED ⓘ |
| subdivision |
Central Rand Group
NERFINISHED
ⓘ
West Rand Group NERFINISHED ⓘ |
| tectonicSetting | stable craton ⓘ |
| thickness | up to 7000 m ⓘ |
| underlies |
Transvaal Supergroup
NERFINISHED
ⓘ
Ventersdorp Supergroup NERFINISHED ⓘ |
Referenced by (5)
Full triples — surface form annotated when it differs from this entity's canonical label.
this entity surface form:
Witwatersrand Basin
this entity surface form:
Witwatersrand Basin
this entity surface form:
Witwatersrand Basin