Damara orogeny

E457101

The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.

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Statements (49)

Predicate Object
instanceOf mountain-building event
orogeny
age Neoproterozoic
early Paleozoic
associatedMineralization base metal deposits
uranium deposits in central Namibia
associatedRockType granitoids
marbles
metasedimentary rocks
metavolcanic rocks
associatedWith Gondwana supercontinent NERFINISHED
assembly of Gondwana
causedBy collision of Congo Craton and Kalahari Craton
continent Gondwana NERFINISHED
developedAlong Damara Belt NERFINISHED
intra-continental mobile belt
endPeriod early Paleozoic
formsPartOf Pan-African–Brasiliano orogenic system NERFINISHED
geodynamicContext Gondwana amalgamation NERFINISHED
involvesCraton Congo Craton NERFINISHED
Kalahari Craton NERFINISHED
Rio de la Plata Craton NERFINISHED
locatedIn Namibia NERFINISHED
Southwestern Africa NERFINISHED
locatedOn African Plate NERFINISHED
metamorphicGrade amphibolite facies
granulite facies
greenschist facies
orogenicBelt Damara Belt NERFINISHED
partOf Pan-African orogeny NERFINISHED
peakActivityApproxMa around 550–500 Ma
precededBy rifting of Rodinia fragments in southwestern Gondwana region
relatedOrogen East African orogeny NERFINISHED
Gariep orogeny NERFINISHED
Kaoko orogeny NERFINISHED
Kuunga orogeny NERFINISHED
resultedIn folding and thrusting of crustal rocks
formation of Damara Belt
granite intrusions in central Namibia
metamorphism of sedimentary basins in Namibia
significance records late Neoproterozoic to early Paleozoic plate convergence in southwestern Gondwana
startPeriod Neoproterozoic NERFINISHED
structuralTrend ENE–WSW
studiedInDiscipline metamorphic petrology
structural geology
tectonics
tectonicProcess continental collision
subduction
tectonicSetting convergent plate margin

Referenced by (1)

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

Pan-African orogeny hasPart Damara orogeny