Baikal orogeny
E473725
Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
All labels observed (2)
| Label | Occurrences |
|---|---|
| Baikal orogeny canonical | 1 |
| Baikalides | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T4859509 — 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: Baikal orogeny Context triple: [Baikal Mountains, orogeny, Baikal 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.
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.
-
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.
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.
-
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.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Baikal orogeny Target entity description: Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
-
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.
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.
-
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.
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.
-
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 |
geological event
ⓘ
mountain-building event ⓘ orogeny ⓘ |
| affects |
Central Asian orogenic belt
ⓘ
linked to:
Central Asian Orogenic Belt
Siberian craton margins ⓘ |
| associatedWith |
Baikal mountain belt
ⓘ
linked to:
Baikal Mountains
Baikalides ⓘ
linked to:
Baikal orogeny
|
| chronologicalPosition | late Precambrian–early Paleozoic ⓘ |
| endTime | early Paleozoic ⓘ |
| geologicalAgeContext |
Cambrian
ⓘ
Neoproterozoic ⓘ
linked to:
Neoproterozoic Era
|
| hasEffect |
crustal thickening
ⓘ
folding and thrusting of crustal rocks ⓘ formation of mountain belts ⓘ granitoid magmatism ⓘ metamorphism of sedimentary sequences ⓘ |
| hasResult |
reworking of Precambrian basement complexes
ⓘ
stabilization of parts of the Siberian continental crust ⓘ |
| hasStratigraphicSignificance |
controls distribution of Neoproterozoic–Cambrian basins
ⓘ
defines regional unconformities in Siberia ⓘ |
| involvesProcess |
continental collision
ⓘ
subduction ⓘ terrane accretion ⓘ |
| namedAfter |
Lake Baikal region
ⓘ
linked to:
Baikal region
|
| occursIn |
Central Asia
ⓘ
Siberia ⓘ |
| partOf |
tectonic evolution of Central Asia
ⓘ
tectonic evolution of Siberia ⓘ |
| precedes | Caledonian orogeny ⓘ |
| produced |
granite intrusions in Siberia
ⓘ
metamorphic belts in Baikal region ⓘ |
| relatedTo |
Cadomian orogeny
ⓘ
Pan-African orogeny ⓘ |
| startTime | late Precambrian ⓘ |
| studiedInDiscipline |
historical geology
ⓘ
structural geology ⓘ tectonics ⓘ |
| tectonicSetting |
accretionary orogeny
ⓘ
continental margin orogeny ⓘ |
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: Baikal orogeny Description of subject: Baikal orogeny is an ancient mountain-building event that shaped parts of Siberia and Central Asia during the late Precambrian to early Paleozoic eras.
Referenced by (2)
Full triples — surface form annotated when it differs from this entity's canonical label.
linked to: Baikal orogeny