Trans-North China Orogen

E781049

The Trans-North China Orogen is a major Paleoproterozoic collisional belt in northern China that records the suturing of ancient continental blocks within the North China Craton.

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Statements (47)

Predicate Object
instanceOf Paleoproterozoic orogen
collisional belt
orogenic belt
ageRange approximately 2.1–1.8 billion years ago
alsoKnownAs Trans-North China Belt NERFINISHED
associatedWith crustal thickening
granitoid magmatism
high-grade regional metamorphism
subduction and collision processes
boundedBy Eastern Block of the North China Craton NERFINISHED
Western Block of the North China Craton NERFINISHED
contains fold-and-thrust structures
high-strain tectonic belts
suture-related shear zones
continent Asia
country China
evidenceFrom geochemistry
geochronology
metamorphic petrology
structural geology
formedBy collision of Archean continental blocks
continental collision
formedDuring Paleoproterozoic Era NERFINISHED
geodynamicRole records assembly of continental lithosphere in the Paleoproterozoic
geologicalAge Paleoproterozoic NERFINISHED
links Eastern Block of the North China Craton NERFINISHED
Western Block of the North China Craton NERFINISHED
lithology granitoid intrusions
high-grade metamorphic rocks
volcanic-sedimentary sequences
locatedIn northern China
metamorphicGrade amphibolite facies
granulite facies
orientation generally northeast–southwest trending
orogenType collisional
partOf North China Craton NERFINISHED
records Paleoproterozoic subduction-accretion processes
continental growth of the North China Craton
suturing of ancient continental blocks within the North China Craton
researchField Precambrian geology
metamorphic petrology
tectonics
significance key to understanding early Proterozoic tectonics in East Asia
tectonicProcess cratonization of the North China Craton
tectonicSetting collisional orogen
tectonicSignificance records assembly of the North China Craton
represents a major Paleoproterozoic suture zone

Referenced by (1)

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

North China Craton hasSubdivision Trans-North China Orogen