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.

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Statements (34)

Predicate Object
instanceOf geological subprovince
tectonostratigraphic terrane
hasBasement Precambrian basement rocks
hasCrustalAffinity Kalahari Craton NERFINISHED
hasCrustalEvolution polyphase
hasGeochronology Mesoproterozoic metamorphic ages
Paleoproterozoic crustal formation ages
hasGeologicalAge Precambrian NERFINISHED
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 NERFINISHED
Kalahari Craton interior
Namaqua-Natal Belt NERFINISHED
isImportantFor Proterozoic tectonic evolution of southern Africa
reconstruction of Kalahari Craton assembly
isSeparatedFrom Kaapvaal Craton NERFINISHED
locatedIn Namibia NERFINISHED
southern Africa NERFINISHED
partOf Kalahari Craton NERFINISHED

Referenced by (1)

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

Kalahari Craton contains Rehoboth Subprovince