Andean orogeny

E55294

The Andean orogeny is the long-lasting mountain-building process responsible for creating and uplifting the Andes Mountains along the western margin of South America due to subduction of oceanic plates beneath the continent.

All labels observed (5)

Label Occurrences
Andean orogeny canonical 20
Andean orogenic belt 3
Andean orogenic system 2

How this entity was disambiguated

Statements (51)

Predicate Object
instanceOf geological process
mountain-building process
orogeny
associatedWith Andes
surface form: Andean Cordillera

Andean back-arc basins
Andean foreland
surface form: Andean foreland deformation

Andean seismicity
Andean subduction system
surface form: Benioff zone beneath the Andes
beganDuring Late Jurassic
Mesozoic era
causedBy subduction of oceanic plates beneath South America
subduction of the Antarctic Plate beneath the South American Plate
subduction of the Caribbean Plate beneath northwestern South America
subduction of the Nazca Plate beneath the South American Plate
continuedDuring Cenozoic
surface form: Cenozoic era

Neogene
surface form: Neogene period

Paleogene
surface form: Paleogene period
drivenBy crustal shortening
crustal thickening
oceanic–continental plate convergence
slab pull of subducting oceanic plates
hasPart Bolivian orogenic phase
Chilean orogenic phase
Incaic phase of the Andean orogeny
Andean orogeny self-linksurface differs
surface form: Patagonian orogenic phase

Peruvian phase of the Andean orogeny
Quechua phase of the Andean orogeny
influencedBy changes in subduction angle
flat-slab subduction segments beneath South America
intensifiedDuring Cretaceous period
isOngoing true
occursIn western margin of South America
partOf Andes Mountains geological history
produced Andean magmatism
Andean volcanism
fold-and-thrust belts in the Andes
foreland basins east of the Andes
high plateau of the Altiplano–Puna
thickened continental crust beneath the Andes
relatedTo Andean Volcanic Belt
surface form: Andean volcanic belt

Andean-type continental margin
resultedIn uplift of the Andes Mountains
spatialExtent Argentina
Bolivia
Chile
Colombia
Ecuador
Patagonia
Peru
Venezuela
tectonicSetting convergent plate boundary

How these facts were elicited

Referenced by (27)

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

Cenozoic includesEvent Andean orogeny
Andes Mountains foothills geologicalRelation Andean orogeny
this entity surface form: Andean orogenic belt
Andean subduction system drives Andean orogeny
Nazca Basin relatedTo Andean orogeny
Andean orogeny hasPart Andean orogeny self-linksurface differs
this entity surface form: Patagonian orogenic phase
San Pedro volcano orogeny Andean orogeny
Nevado de Acay volcanic center orogeny Andean orogeny
Andean Volcanic Belt associatedWith Andean orogeny
Andean Volcanic Belt partOf Andean orogeny
this entity surface form: Andean orogenic system
Tupungatito volcano isPartOf Andean orogeny
subject surface form: Tupungatito
American Cordillera orogenyType Andean orogeny
Andean foreland partOf Andean orogeny
this entity surface form: Andean orogenic system
Andean foreland studiedIn Andean orogeny
this entity surface form: Andean tectonics
Cordillera de Mérida orogeny Andean orogeny
Cordillera Occidental orogeny Andean orogeny
Cordillera Oriental orogeny Andean orogeny
Andean porphyry copper belt relatedTo Andean orogeny
western Argentina tectonicSetting Andean orogeny
subject surface form: Western Argentina
this entity surface form: Andean orogenic belt
Andean back-arc basins associatedWith Andean orogeny
Atacazo orogeny Andean orogeny
Santa Bárbara mine geologicalSetting Andean orogeny
this entity surface form: Andean orogenic belt