Brasiliano orogeny

E457100

The Brasiliano orogeny was a major Neoproterozoic mountain-building event in South America associated with the assembly of the supercontinent Gondwana.

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Statements (48)

Predicate Object
instanceOf Neoproterozoic orogeny
geological event
orogeny
affects Araçuaí Belt NERFINISHED
Borborema Province NERFINISHED
Brasília Belt NERFINISHED
Dom Feliciano Belt NERFINISHED
Mantiqueira Province NERFINISHED
Pampean Belt NERFINISHED
Paraguay Belt NERFINISHED
Precambrian basement of Brazil
Ribeira Belt NERFINISHED
Sierras Pampeanas NERFINISHED
South American Platform NERFINISHED
São Francisco Craton margins
Tocantins Province NERFINISHED
approximateAgeMa 900–500 Ma
associatedWith Gondwana assembly NERFINISHED
supercontinent cycle
cause closure of Neoproterozoic ocean basins
collision of cratonic blocks in South America
continent South America
correlatesWith Pan-African orogeny in Africa NERFINISHED
country Argentina
Bolivia
Brazil
Paraguay NERFINISHED
Uruguay NERFINISHED
endTime Neoproterozoic
fieldOfStudy Precambrian geology
structural geology
tectonics
geologicalPeriod Neoproterozoic NERFINISHED
linkedTo Pan-African orogeny NERFINISHED
orogenicCycle Brasiliano–Pan-African orogenic cycle NERFINISHED
overprints older Precambrian structures
partOf assembly of Gondwana
precedes breakup of Gondwana NERFINISHED
relatedProcess accretion of terranes
continental collision
subduction
resultedIn crustal thickening
formation of Neoproterozoic mobile belts in South America
granitoid magmatism
metamorphism of Precambrian rocks
shear zones and thrust belts
startTime Neoproterozoic
tectonicSetting collisional orogeny

Referenced by (2)

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

Pannotia associatedOrogeny Brasiliano orogeny
Pan-African orogeny hasPart Brasiliano orogeny