Qinling–Dabie orogeny

E404173

geological event mountain-building event orogeny

The Qinling–Dabie orogeny was a major Paleozoic–Mesozoic mountain-building event in central China that formed the Qinling and Dabie mountain ranges through the collision of the North China and South China tectonic blocks.

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All labels observed (4)

Label	Occurrences
Qinling–Dabie orogenic belt	3
Qinling–Dabie–Sulu orogenic belt	2
Qinling–Dabie belt	1
Qinling–Dabie orogeny canonical	1

How this entity was disambiguated

This entity first appeared as the object of triple T3992897 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.

NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07

Target entity: Qinling–Dabie orogeny
Context triple: [Dabie Mountains, orogeny, Qinling–Dabie orogeny]

A. Yanshanian orogeny
The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
B. Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
C. Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
D. Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
E. Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
F. None of above. chosen
G. Unsure - the case is ambiguous/there is not enough information to decide.

NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07

Target entity: Qinling–Dabie orogeny
Target entity description: The Qinling–Dabie orogeny was a major Paleozoic–Mesozoic mountain-building event in central China that formed the Qinling and Dabie mountain ranges through the collision of the North China and South China tectonic blocks.

A. Yanshanian orogeny
The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
B. Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
C. Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
D. Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
E. Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
F. None of above. chosen

Statements (47)

Predicate	Object
instanceOf	geological event ⓘ mountain-building event ⓘ orogeny ⓘ
associatedRockType	eclogite ⓘ gneiss ⓘ granite ⓘ
associatedStructure	Dabie suture zone ⓘ linked to: Qinling suture zone Qinling suture zone ⓘ
associatedWith	eclogite-facies metamorphism ⓘ granitoid magmatism ⓘ high-pressure metamorphic rocks ⓘ suture zone between North China and South China blocks ⓘ ultrahigh-pressure metamorphism ⓘ
causedBy	collision of the North China Block and South China Block ⓘ
continent	Asia ⓘ
country	China ⓘ
deformationStyle	crustal thickening ⓘ thrusting and folding ⓘ
endEra	Mesozoic Era ⓘ
formed	Dabie Mountains ⓘ Qinling Mountains ⓘ
geologicalPeriod	Mesozoic ⓘ Paleozoic ⓘ
hasPhase	continental collision ⓘ post-collisional extension ⓘ subduction-related deformation ⓘ
locatedIn	central China ⓘ linked to: Central China
metamorphicGrade	high-pressure ⓘ ultrahigh-pressure ⓘ
orogen	Qinling–Dabie orogenic belt ⓘ linked to: Qinling–Dabie orogeny
plateInvolved	North China Block ⓘ South China Block ⓘ
region	Qinling–Dabie belt ⓘ linked to: Qinling–Dabie orogeny
relatedTo	Qinling–Dabie–Sulu orogenic belt ⓘ linked to: Qinling–Dabie orogeny Sino-Korean Craton ⓘ linked to: North China Craton Yangtze Craton ⓘ linked to: Yangtze Plate
researchField	metamorphic petrology ⓘ structural geology ⓘ tectonics ⓘ
resultedIn	amalgamation of the North China Block and South China Block ⓘ closure of the Paleo-Tethys-related oceanic basin between North China and South China blocks ⓘ formation of the Qinling–Dabie–Sulu orogenic belt ⓘ
significance	important for understanding continental collision processes ⓘ key event in the tectonic evolution of East Asia ⓘ records deep subduction of continental crust ⓘ
startEra	Paleozoic Era ⓘ
tectonicSetting	continental collision ⓘ

How these facts were elicited