Central Asian Orogenic Belt

E781044

The Central Asian Orogenic Belt is a vast, geologically complex mountain-building region in Eurasia formed by the long-term collision and accretion of multiple continental and oceanic terranes.

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Observed surface forms (1)

Statements (48)

Predicate Object
instanceOf geological region
orogenic belt
alsoKnownAs Altaid Tectonic Collage NERFINISHED
Central Asian Fold Belt NERFINISHED
closedOcean Paleo-Asian Ocean NERFINISHED
contains Altai Mountains NERFINISHED
Junggar region NERFINISHED
Kazakh orocline NERFINISHED
Mongolian Altai NERFINISHED
Tianshan Mountains NERFINISHED
continent Asia
Europe
extendsAcross Central Asia NERFINISHED
Kazakhstan NERFINISHED
Mongolia NERFINISHED
northwestern China
southern Siberia NERFINISHED
extendsFrom Ural Mountains NERFINISHED
extendsTo Pacific margin
formationBegan Neoproterozoic era NERFINISHED
formedBy accretion of oceanic terranes
collision of continental terranes
subduction-related processes
geologicalAge Neoproterozoic NERFINISHED
Paleozoic NERFINISHED
hasProcess continental collision
crustal thickening
strike-slip faulting
subduction
knownFor abundant granitoid magmatism
complex tectonic history
large-scale crustal growth
significant mineral resources
lithology metamorphic rocks
plutonic rocks
sedimentary rocks
volcanic rocks
locatedIn Eurasia NERFINISHED
majorGrowth Paleozoic era NERFINISHED
orogenyType accretionary orogen
partOf Asian highlands
researchField geodynamics
metallogeny
tectonics
tectonicSetting accretionary complexes
island arcs
multiple microcontinents
oceanic plateaus

Referenced by (3)

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

Siberian Craton boundedBy Central Asian Orogenic Belt
North China Craton borderedBy Central Asian Orogenic Belt
Chinese continental crust hasPart Central Asian Orogenic Belt
this entity surface form: Central Asian Orogenic Belt segments in northern China