Sveconorwegian orogeny
E542420
The Sveconorwegian orogeny was a major Mesoproterozoic mountain-building event that shaped much of southwestern Scandinavia, forming part of the ancient basement rocks of the Fennoscandian region.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Sveconorwegian orogeny canonical | 2 |
How this entity was disambiguated
This entity first appeared as the object of triple T5655777 — 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.
Target entity: Sveconorwegian orogeny Context triple: [Fennoscandian Shield, orogenicHistory, Sveconorwegian orogeny]
-
A.
Svecofennian orogeny
The Svecofennian orogeny was a major Paleoproterozoic mountain-building event that formed much of the continental crust of present-day Sweden and Finland within the Fennoscandian Shield.
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B.
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.
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C.
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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D.
Karelian orogeny
The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
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E.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Sveconorwegian orogeny Target entity description: The Sveconorwegian orogeny was a major Mesoproterozoic mountain-building event that shaped much of southwestern Scandinavia, forming part of the ancient basement rocks of the Fennoscandian region.
-
A.
Svecofennian orogeny
The Svecofennian orogeny was a major Paleoproterozoic mountain-building event that formed much of the continental crust of present-day Sweden and Finland within the Fennoscandian Shield.
-
B.
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.
-
C.
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.
-
D.
Karelian orogeny
The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
-
E.
Caledonian orogeny
The Caledonian orogeny was a major Paleozoic mountain-building event that formed ranges across what are now Scandinavia, Scotland, Ireland, Greenland, and parts of North America as ancient continents collided.
- F. None of above. chosen
Statements (46)
| Predicate | Object |
|---|---|
| instanceOf |
Mesoproterozoic orogeny
ⓘ
geological event ⓘ orogeny ⓘ |
| affects |
Baltic Shield
NERFINISHED
ⓘ
Fennoscandian basement NERFINISHED ⓘ |
| associatedWith |
large-scale ductile deformation
ⓘ
partial melting of crust ⓘ shear zones in southwestern Scandinavia ⓘ |
| causedBy |
continental collision
ⓘ
crustal shortening ⓘ thickening of continental crust ⓘ |
| continent | Europe ⓘ |
| duration | approximately 240 million years ⓘ |
| endTime | approximately 0.90 billion years ago ⓘ |
| forms |
basement rocks of southwestern Scandinavia
ⓘ
gneiss complexes ⓘ granulite-facies rocks ⓘ high-grade metamorphic rocks ⓘ migmatites ⓘ |
| geologicalPeriod | Mesoproterozoic ⓘ |
| includesPhase |
early accretionary phase
ⓘ
late extensional and exhumation phase ⓘ main collisional phase ⓘ |
| locatedIn |
Norway
ⓘ
Sweden ⓘ southwestern Scandinavia ⓘ |
| namedAfter | Sveconorwegian Province NERFINISHED ⓘ |
| orogenyType | collisional orogeny ⓘ |
| partOf | Fennoscandian Shield NERFINISHED ⓘ |
| peakMetamorphism | high-grade amphibolite to granulite facies ⓘ |
| precededBy | Gothian orogeny NERFINISHED ⓘ |
| produced |
Sveconorwegian gneiss domes
ⓘ
syn-orogenic granites ⓘ |
| relatedTo | Grenvillian orogeny NERFINISHED ⓘ |
| researchField |
Precambrian geology
ⓘ
metamorphic petrology ⓘ tectonics ⓘ |
| result |
deformation of pre-existing crust
ⓘ
granitoid magmatism ⓘ mountain belt formation in southwestern Fennoscandia ⓘ regional metamorphism ⓘ |
| significance |
key event in Proterozoic assembly of southwestern Baltica
ⓘ
major crust-forming event in Fennoscandia ⓘ |
| startTime | approximately 1.14 billion years ago ⓘ |
| tectonicSetting | margin of the Fennoscandian Shield ⓘ |
| temporalCorrelation | Grenvillian orogeny NERFINISHED ⓘ |
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.
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.
Subject: Sveconorwegian orogeny Description of subject: The Sveconorwegian orogeny was a major Mesoproterozoic mountain-building event that shaped much of southwestern Scandinavia, forming part of the ancient basement rocks of the Fennoscandian region.
Referenced by (2)
Full triples — surface form annotated when it differs from this entity's canonical label.