Rehoboth Subprovince

E786459

The Rehoboth Subprovince is a geological region forming part of the ancient Kalahari Craton in southern Africa, characterized by its Precambrian basement rocks and complex tectonic history.

All labels observed (1)

Label Occurrences
Rehoboth Subprovince canonical 1

How this entity was disambiguated

Statements (34)

Predicate Object
instanceOf geological subprovince
tectonostratigraphic terrane
hasBasement Precambrian basement rocks
hasCrustalAffinity Kalahari Craton
hasCrustalEvolution polyphase
hasGeochronology Mesoproterozoic metamorphic ages
Paleoproterozoic crustal formation ages
hasGeologicalAge Precambrian
hasLithology granitoid rocks
metasedimentary rocks
metavolcanic rocks
hasMagmatism Proterozoic granitoid intrusions
mafic dykes
hasMetamorphicGrade low- to medium-grade metamorphism
hasResearchDiscipline Precambrian geology
geochronology
structural geology
tectonics
hasStructuralStyle fold-and-thrust structures
shear zones
hasTectonicEvents Mesoproterozoic reworking
Neoproterozoic overprinting
Paleoproterozoic orogenesis
hasTectonicHistory complex
hasTectonicSetting intra-cratonic
isBoundedBy Damara Belt
Kalahari Craton interior
Namaqua-Natal Belt
isImportantFor Proterozoic tectonic evolution of southern Africa
reconstruction of Kalahari Craton assembly
isSeparatedFrom Kaapvaal Craton
locatedIn Namibia
southern Africa
linked to: Southern Africa
partOf Kalahari Craton

How these facts were elicited

Referenced by (1)

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

Kalahari Craton contains Rehoboth Subprovince