Yanshanian orogeny
E322687
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.
All labels observed (3)
| Label | Occurrences |
|---|---|
| Yanshanian magmatism | 1 |
| Yanshanian orogeny canonical | 1 |
| Yanshanian tectonic phase | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T3061687 — 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: Yanshanian orogeny Context triple: [Yan Mountains, orogeny, Yanshanian orogeny]
-
A.
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.
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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.
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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D.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
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E.
Himalayan orogeny
The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Yanshanian orogeny Target entity description: 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.
-
A.
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.
-
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.
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.
-
D.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
-
E.
Himalayan orogeny
The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
- F. None of above. chosen
Statements (44)
| Predicate | Object |
|---|---|
| instanceOf |
Mesozoic tectonic event
ⓘ
geological event ⓘ orogeny ⓘ |
| affects |
North China Craton
ⓘ
Yan Mountains ⓘ |
| associatedWith |
Yanshanian orogeny
self-linksurface differs
ⓘ
surface form:
Yanshanian magmatism
Yanshanian orogeny self-linksurface differs ⓘ
surface form:
Yanshanian tectonic phase
|
| causedBy |
subduction-related tectonics
ⓘ
tectonic compression ⓘ |
| chronology |
Cretaceous extensional overprint
ⓘ
early Jurassic deformation phase ⓘ late Jurassic deformation phase ⓘ multi-stage tectonic evolution ⓘ |
| country | China ⓘ |
| deformationStyle |
compressional
ⓘ
transpressional ⓘ |
| endTime | Cretaceous ⓘ |
| fieldOfStudy |
orogenic processes
ⓘ
structural geology ⓘ tectonics ⓘ |
| geologicalPeriod |
Mesozoic Era
ⓘ
surface form:
Mesozoic
|
| influences |
basin-and-range style structures in northern China
ⓘ
distribution of Mesozoic volcanic rocks in North China ⓘ |
| locatedIn | northern China ⓘ |
| namedAfter | Yan Mountains ⓘ |
| overprints | older Paleozoic structures in North China Craton ⓘ |
| partOf | Mesozoic tectonic evolution of East Asia ⓘ |
| process |
crustal shortening
ⓘ
folding ⓘ granitoid intrusion ⓘ magmatism ⓘ thrust faulting ⓘ |
| region |
North China
ⓘ
Northeast Asia ⓘ |
| result |
development of large-scale faults
ⓘ
formation of sedimentary basins ⓘ mountain building ⓘ reconfiguration of regional stress field ⓘ rejuvenation of North China Craton margins ⓘ uplift of Yan Mountains ⓘ |
| significance |
important for mineralization and ore formation in northern China
ⓘ
key event in the tectonic evolution of the North China Craton ⓘ major Mesozoic mountain-building event in northern China ⓘ |
| startTime | Jurassic ⓘ |
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: Yanshanian orogeny Description of subject: 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.
Referenced by (3)
Full triples — surface form annotated when it differs from this entity's canonical label.