Gariep Belt

E786465

The Gariep Belt is a Neoproterozoic to early Paleozoic orogenic belt in southwestern Africa, marking a major tectonic suture along the margin of the Kalahari Craton.

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Statements (46)

Predicate Object
instanceOf Neoproterozoic orogen
geological formation
orogenic belt
ageRangeMa ca. 650–500 Ma
associatedWith deformation
metamorphism
subduction-related magmatism
borders Kalahari Craton NERFINISHED
boundedBy Kalahari Craton to the east
paleo-oceanic domain to the west
contains accretionary prism sequences
back-arc basin deposits
fore-arc basin deposits
country Namibia
South Africa
evidenceFor assembly of Gondwana
exposedIn Namaqualand region NERFINISHED
southwestern Namibia NERFINISHED
formedBy continental collision
ocean closure
formedDuring Pan-African–Brasiliano orogenic cycle NERFINISHED
geologicalAge Neoproterozoic NERFINISHED
early Paleozoic
hasLithology granitoid intrusions
metasedimentary rocks
metavolcanic rocks
ophiolitic fragments
hasMetamorphicGrade low-grade metamorphism
medium-grade metamorphism
hasSignificance records Neoproterozoic plate convergence along Kalahari margin
hasStructuralStyle fold-and-thrust belt
imbricate thrust stacking
locatedIn southwestern Africa NERFINISHED
marks major tectonic suture
namedAfter Gariep (Orange) River region NERFINISHED
orientedAlong southwest margin of Kalahari Craton
overlies Kalahari Craton margin NERFINISHED
partOf Pan-African orogenic system NERFINISHED
relatedTo Damara Belt NERFINISHED
Saldania Belt NERFINISHED
researchField geochronology
metamorphic petrology
structural geology
tectonics
tectonicEnvironment active continental margin
tectonicSetting Pan-African orogeny NERFINISHED

Referenced by (1)

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

Kalahari Craton boundedBy Gariep Belt