Andean subduction system

E50874

The Andean subduction system is a major tectonic convergent margin along western South America where an oceanic plate descends beneath the continent, driving Andean mountain building, volcanism, and seismic activity.


Statements (50)
Predicate Object
instanceOf convergent plate margin
subduction zone
tectonic system
activeDuring Cenozoic
associatedWith Andean volcanic arc
Andes Mountains
Austral Volcanic Zone of the Andes
Central Volcanic Zone of the Andes
Northern Volcanic Zone of the Andes
Peru–Chile Trench
Peru–Chile megathrust
Southern Volcanic Zone of the Andes
copper ore deposits in the Andes
porphyry copper systems
skarn deposits
boundedBy Nazca Plate to the west
South American continental interior to the east
causes arc volcanism in the Andes
seismic activity in the Andes
controls distribution of Andean volcanism
topography of the Andes
drives Andean mountain building
Andean orogeny
extendsFrom Venezuela
extendsTo Tierra del Fuego
hasFeature flat-slab segments
steep-slab segments
hasOverridingPlate South American Plate
hasProcess arc magmatism
back-arc extension in some segments
forearc deformation
mantle wedge hydration
oceanic lithosphere subduction
hasSubductingPlate Antarctic Plate
Nazca Plate
influences Andean back-arc deformation
Andean climate patterns
Andean foreland basins
Andean mineralization
initiated Mesozoic
locatedIn western margin of South America
marginType oceanic–continental convergent margin
produces crustal shortening in the Andes
crustal thickening beneath the Andes
megathrust earthquakes
tsunamigenic earthquakes
studiedIn plate tectonics
seismology
structural geology
volcanology

Referenced by (4)
Subject (surface form when different) Predicate
Andean orogeny ("Benioff zone beneath the Andes")
Peru–Chile Trench region ("Benioff seismic zone beneath South America")
associatedWith
Andean subduction system ("Andean back-arc deformation")
influences
Nazca Plate
partOfSystem

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