Triple
T16575132
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Arkoma Basin |
E402689
|
entity |
| Predicate | relatedTo |
P37
|
FINISHED |
| Object | Ouachita orogeny |
E92147
|
NE FINISHED |
Disambiguation candidates (1 decision)
The exact options the model was shown at each disambiguation step, with the option it chose highlighted — the evidence behind this triple's disambiguated ids.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Ouachita orogeny Context triple: [Arkoma Basin, relatedTo, Ouachita orogeny]
-
A.
Ouachita orogeny
chosen
The Ouachita orogeny was a major Paleozoic mountain-building event that formed the Ouachita Mountains of Arkansas, Oklahoma, and adjacent regions through the collision of ancient continental plates.
-
B.
Sevier orogeny
The Sevier orogeny was a major Mesozoic mountain-building event in western North America that produced extensive thrust faulting and deformation along the continental margin.
-
C.
Acadian orogeny
The Acadian orogeny was a major Middle Paleozoic mountain-building event that significantly shaped the northern Appalachian Mountains through the collision of ancient landmasses.
-
D.
Appalachian orogeny
The Appalachian orogeny was a series of ancient mountain-building events that formed the Appalachian Mountains through the collision of tectonic plates during the Paleozoic Era.
-
E.
Wopmay orogeny
Wopmay orogeny was a Paleoproterozoic mountain-building event that deformed the western margin of the ancient North American craton, providing key evidence for early plate tectonic processes.
- F. None of above.
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Provenance (3 batches)
| Stage | Batch ID | Job type | Status |
|---|---|---|---|
| creating | batch_69d88387363c8190a97a0c942130de97 |
elicitation | completed |
| NER | batch_69e3595bbbbc8190b023f4872908c031 |
ner | completed |
| NED1 | batch_6a006eea409c8190808170a0b3f4bd17 |
ned_source_triple | completed |
Created at: April 10, 2026, 5:16 a.m.