Taimyr Orogen
E781776
The Taimyr Orogen is a major Paleozoic mountain belt in the Taimyr Peninsula of Arctic Siberia, formed by tectonic collisions along the northern margin of the Siberian Craton.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Taimyr Orogen canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T9143183 — 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: Taimyr Orogen Context triple: [Siberian Craton, boundedBy, Taimyr Orogen]
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A.
Grenville orogenic belt
The Grenville orogenic belt is a vast, ancient mountain-building region in eastern North America and beyond, formed over a billion years ago and representing one of the major Precambrian collisional events in Earth’s history.
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B.
Cape Fold Belt
The Cape Fold Belt is a mountain range system in southwestern South Africa characterized by folded sedimentary rocks and dramatic parallel ridges formed during the Paleozoic–Mesozoic era.
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C.
Baikal orogeny
Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
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D.
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.
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E.
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.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Taimyr Orogen Target entity description: The Taimyr Orogen is a major Paleozoic mountain belt in the Taimyr Peninsula of Arctic Siberia, formed by tectonic collisions along the northern margin of the Siberian Craton.
-
A.
Grenville orogenic belt
The Grenville orogenic belt is a vast, ancient mountain-building region in eastern North America and beyond, formed over a billion years ago and representing one of the major Precambrian collisional events in Earth’s history.
-
B.
Cape Fold Belt
The Cape Fold Belt is a mountain range system in southwestern South Africa characterized by folded sedimentary rocks and dramatic parallel ridges formed during the Paleozoic–Mesozoic era.
-
C.
Baikal orogeny
Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
-
D.
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.
-
E.
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.
- F. None of above. chosen
Statements (39)
| Predicate | Object |
|---|---|
| instanceOf |
geologic province
ⓘ
mountain belt ⓘ orogen ⓘ |
| associatedWith | Siberian Craton NERFINISHED ⓘ |
| boundedBy | Siberian Craton to the south ⓘ |
| contains |
deformed sedimentary rocks
ⓘ
igneous intrusions ⓘ metamorphic rocks ⓘ |
| evidenceFrom |
field mapping
ⓘ
geochronology ⓘ petrology ⓘ structural analysis ⓘ |
| extendsAcross | central Taimyr Peninsula NERFINISHED ⓘ |
| formedBy |
plate convergence
ⓘ
tectonic collisions ⓘ |
| geologicPeriod | Paleozoic NERFINISHED ⓘ |
| hasImportanceFor |
reconstructing Paleozoic paleogeography of Siberia
ⓘ
understanding the assembly of Arctic continental blocks ⓘ |
| hasTectonicStyle |
crustal shortening
ⓘ
folding ⓘ thrusting ⓘ |
| isInContinent | Asia NERFINISHED ⓘ |
| isInCountry | Russia NERFINISHED ⓘ |
| isInRegion | Russian Arctic NERFINISHED ⓘ |
| locatedIn |
Arctic Siberia
NERFINISHED
ⓘ
Taimyr Peninsula NERFINISHED ⓘ |
| locatedOn | northern margin of the Siberian Craton ⓘ |
| marginType | northern passive-to-active margin of the Siberian Craton ⓘ |
| minimumAge | Paleozoic ⓘ |
| orogenyAge | Paleozoic ⓘ |
| overprints | older basement of the Siberian Craton margin ⓘ |
| partOf | Siberian Arctic orogenic systems NERFINISHED ⓘ |
| relatedTo |
Arctic orogenic belts
NERFINISHED
ⓘ
Paleozoic plate reconstructions of the Arctic ⓘ |
| researchField |
regional geology
ⓘ
structural geology ⓘ tectonics ⓘ |
| significance | records Paleozoic tectonic evolution of the northern Siberian margin ⓘ |
| tectonicSetting | collisional orogen ⓘ |
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: Taimyr Orogen Description of subject: The Taimyr Orogen is a major Paleozoic mountain belt in the Taimyr Peninsula of Arctic Siberia, formed by tectonic collisions along the northern margin of the Siberian Craton.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.