Marathon orogeny
E402691
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.
All labels observed (2)
| Label | Occurrences |
|---|---|
| Marathon orogen | 1 |
| Marathon orogeny canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T3946005 — 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: Marathon orogeny Context triple: [Ouachita orogeny, relatedTo, Marathon orogeny]
-
A.
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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B.
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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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.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
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E.
Cascadian orogeny
The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Marathon orogeny Target entity description: 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.
-
A.
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.
-
B.
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.
-
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.
Taconic orogeny
The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
-
E.
Cascadian orogeny
The Cascadian orogeny is the long-lasting mountain-building episode responsible for forming the Cascade Range through subduction-related tectonic activity along western North America.
- F. None of above. chosen
Statements (32)
| Predicate | Object |
|---|---|
| instanceOf |
geological event
ⓘ
mountain-building event ⓘ orogeny ⓘ |
| age | approximately 320–270 million years ago ⓘ |
| associatedWith | assembly of the supercontinent Pangaea ⓘ |
| cause | collision of continental plates ⓘ |
| continent |
Gondwana
ⓘ
Laurentia ⓘ |
| deforms | Paleozoic sedimentary rocks ⓘ |
| geologicalPeriod |
Late Paleozoic
ⓘ
Pennsylvanian ⓘ Permian Period ⓘ
surface form:
Permian
|
| locatedIn |
United States of America
ⓘ
surface form:
United States
western Texas ⓘ |
| orogenicBelt | Marathon fold-and-thrust belt ⓘ |
| overprints | earlier passive-margin strata ⓘ |
| partOf |
Ouachita orogeny
ⓘ
surface form:
Ouachita orogenic belt
late Paleozoic orogenies of North America ⓘ |
| preservedIn |
Marathon Basin
ⓘ
Trans-Pecos region ⓘ
surface form:
Trans-Pecos Texas
|
| relatedTo |
Appalachian orogeny
ⓘ
surface form:
Alleghanian orogeny
Ouachita orogeny ⓘ Variscan orogeny ⓘ |
| researchField |
regional geology of Texas
ⓘ
structural geology ⓘ tectonics ⓘ |
| resultedIn |
crustal shortening
ⓘ
fold-and-thrust deformation of Paleozoic strata ⓘ uplift of the Marathon region ⓘ |
| significance | records late stages of Pangaea assembly in southern Laurentia ⓘ |
| structuralStyle | thin-skinned tectonics ⓘ |
| tectonicSetting | convergent plate margin ⓘ |
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: Marathon orogeny Description of subject: 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.
Referenced by (2)
Full triples — surface form annotated when it differs from this entity's canonical label.