Kuunga orogeny
E461991
The Kuunga orogeny was a late Neoproterozoic to early Paleozoic mountain-building event associated with the final assembly of the Gondwana supercontinent, particularly involving collisions along the margins of East and West Gondwana.
All labels observed (2)
| Label | Occurrences |
|---|---|
| Kuunga orogeny canonical | 2 |
| Gondwanide orogeny | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T4648332 — 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: Kuunga orogeny Context triple: [Pan-African orogeny, hasPart, Kuunga orogeny]
-
A.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
-
B.
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.
-
C.
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.
-
D.
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.
-
E.
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.
- 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: Kuunga orogeny Target entity description: The Kuunga orogeny was a late Neoproterozoic to early Paleozoic mountain-building event associated with the final assembly of the Gondwana supercontinent, particularly involving collisions along the margins of East and West Gondwana.
-
A.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
-
B.
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.
-
C.
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.
-
D.
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.
-
E.
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.
- F. None of above. chosen
Statements (41)
| Predicate | Object |
|---|---|
| instanceOf |
geological event
ⓘ
mountain-building event ⓘ orogeny ⓘ |
| affects | Precambrian basement terranes ⓘ |
| associatedWith |
East Gondwana
NERFINISHED
ⓘ
Gondwana supercontinent NERFINISHED ⓘ West Gondwana NERFINISHED ⓘ |
| chronologicalPosition |
early Paleozoic orogeny
ⓘ
late Neoproterozoic orogeny ⓘ |
| endTime | early Paleozoic ⓘ |
| forms | Kuunga orogenic belt NERFINISHED ⓘ |
| geodynamicContext | closure of ocean basins between Gondwana fragments ⓘ |
| hasEffect |
continental collision
ⓘ
crustal deformation ⓘ metamorphism ⓘ mountain belt formation ⓘ |
| hasLithology |
granitoid intrusions
ⓘ
high-grade metamorphic rocks ⓘ |
| hasOutcome |
formation of long-lived crustal shear zones
ⓘ
suturing of Gondwana blocks ⓘ |
| hasProcess |
folding
ⓘ
regional metamorphism ⓘ thrusting ⓘ |
| involves | collision of East Gondwana and West Gondwana margins ⓘ |
| locatedIn |
Antarctica
ⓘ
Australia ⓘ East Africa NERFINISHED ⓘ India ⓘ Madagascar region NERFINISHED ⓘ |
| namedAfter | Kuunga belt NERFINISHED ⓘ |
| occursIn |
Neoproterozoic
NERFINISHED
ⓘ
Paleozoic ⓘ |
| partOf | assembly of Gondwana NERFINISHED ⓘ |
| playsRoleIn | final amalgamation of Gondwana ⓘ |
| recordedIn | metamorphic belts of East Gondwana margin ⓘ |
| relatedTo |
East African orogeny
NERFINISHED
ⓘ
Pan-African orogeny NERFINISHED ⓘ |
| startTime | late Neoproterozoic ⓘ |
| supercontinentCycleStage | final assembly of Gondwana ⓘ |
| tectonicSetting | collisional orogeny ⓘ |
| timeApproximation | circa 570–530 million years ago ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
Instruction
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Input
Subject: Kuunga orogeny Description of subject: The Kuunga orogeny was a late Neoproterozoic to early Paleozoic mountain-building event associated with the final assembly of the Gondwana supercontinent, particularly involving collisions along the margins of East and West Gondwana.
Referenced by (3)
Full triples — surface form annotated when it differs from this entity's canonical label.
this entity surface form:
Gondwanide orogeny