Wopmay orogeny
E542694
Wopmay orogeny was a Paleoproterozoic mountain-building event that deformed the western margin of the ancient North American craton, providing key evidence for early plate tectonic processes.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Wopmay orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T5605043 — 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: Wopmay orogeny Context triple: [Laurentia, experienced, Wopmay 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.
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C.
Kuunga orogeny
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.
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D.
Sevier orogeny
The Sevier orogeny was a major Mesozoic mountain-building event in western North America that produced extensive thrust faulting and deformation along the continental margin.
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E.
Marathon orogeny
The Marathon orogeny was a late Paleozoic mountain-building event in what is now western Texas, associated with the collision of continental plates during the assembly of the supercontinent Pangaea.
- 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: Wopmay orogeny Target entity description: Wopmay orogeny was a Paleoproterozoic mountain-building event that deformed the western margin of the ancient North American craton, providing key evidence for early plate tectonic processes.
-
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.
Kuunga orogeny
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.
-
D.
Sevier orogeny
The Sevier orogeny was a major Mesozoic mountain-building event in western North America that produced extensive thrust faulting and deformation along the continental margin.
-
E.
Marathon orogeny
The Marathon orogeny was a late Paleozoic mountain-building event in what is now western Texas, associated with the collision of continental plates during the assembly of the supercontinent Pangaea.
- F. None of above. chosen
Statements (43)
| Predicate | Object |
|---|---|
| instanceOf |
geological event
ⓘ
orogeny ⓘ |
| affectedRegion |
Northwest Territories, Canada
ⓘ
linked to:
Northwest Territories
northwestern Canadian Shield ⓘ |
| continentAffected |
Laurentia
ⓘ
North American craton ⓘ
linked to:
Laurentian craton
|
| country | Canada ⓘ |
| deformed |
western margin of the Archean Slave craton
ⓘ
western margin of the North American craton ⓘ |
| endTime | approximately 1.88 billion years ago ⓘ |
| geologicalAge | Paleoproterozoic ⓘ |
| hasComponent |
Coronation margin
ⓘ
Great Bear magmatic zone ⓘ Hottah terrane ⓘ Wopmay fault zone ⓘ |
| hasProcess |
crustal shortening
ⓘ
folding ⓘ magmatism ⓘ metamorphism ⓘ thrust faulting ⓘ |
| hasSignificance |
constrains timing of early plate convergence on Earth
ⓘ
helps reconstruct early Proterozoic configuration of Laurentia ⓘ key example of Paleoproterozoic orogenic systems ⓘ |
| hasTectonicSetting |
continental margin orogeny
ⓘ
plate collision ⓘ |
| hostRockAge | Archean basement ⓘ |
| isExampleOf |
Proterozoic mountain-building event
ⓘ
early Proterozoic continental assembly ⓘ |
| isOverlainBy | younger Proterozoic sedimentary sequences ⓘ |
| namedAfter | Wopmay River ⓘ |
| orogenType | collisional orogen ⓘ |
| overprints | older Archean structures ⓘ |
| partOf | Proterozoic orogenies ⓘ |
| providesEvidenceFor |
Proterozoic plate convergence
ⓘ
Wilson cycle processes in the Paleoproterozoic ⓘ early plate tectonics ⓘ |
| resultedIn |
development of foreland basin deposits
ⓘ
formation of a Paleoproterozoic mountain belt ⓘ thickening of continental crust ⓘ |
| startTime | approximately 1.97 billion years ago ⓘ |
| studiedInDiscipline |
Precambrian geology
ⓘ
structural geology ⓘ tectonics ⓘ |
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: Wopmay orogeny Description of subject: Wopmay orogeny was a Paleoproterozoic mountain-building event that deformed the western margin of the ancient North American craton, providing key evidence for early plate tectonic processes.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.