Andean orogeny

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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.


Statements (51)
Predicate Object
instanceOf geological process
mountain-building process
orogeny
associatedWith Andean Cordillera
Andean back-arc basins
Andean foreland deformation
Andean seismicity
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 era
Neogene period
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
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
Andean-type continental margin
resultedIn uplift of the Andes Mountains
spatialExtent Argentina
Bolivia
Chile
Colombia
Ecuador
Patagonia
Peru
Venezuela
tectonicSetting convergent plate boundary


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