Triple
T19673640
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Caucasus volcanic arc |
E472395
|
entity |
| Predicate | associatedWith |
P37
|
FINISHED |
| Object | Caucasus orogeny |
—
|
NE NERFINISHED |
How this triple was built (2 steps)
Every LLM step that produced this triple, in pipeline order — named-entity classification, the disambiguation choices (the exact options shown, with the pick highlighted), and the generated description. The batch + timestamp of each is in the Provenance table below.
NER
Named-entity recognition
gpt-5-mini
Instruction
Given a phrase, classify it is english named entity (e.g., persons, organizations, works of art) in Latin script, or not (e.g., literals, dates, URLs, verbose phrases). For disambiguation, the statement where the phrase occurs as object is also given. Please return a JSON object with `phrase` (string, the phrase being analyzed) and `is_ne` (boolean, indicating whether the phrase is a Named Entity).
Input
Phrase: Caucasus orogeny | Statement: [Caucasus volcanic arc, associatedWith, Caucasus orogeny]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Caucasus orogeny Context triple: [Caucasus volcanic arc, associatedWith, Caucasus orogeny]
-
A.
Caucasus orogeny
chosen
The Caucasus orogeny is the mountain-building event responsible for forming the Caucasus region through the collision of tectonic plates between the Black and Caspian Seas.
-
B.
Carpathian orogeny
The Carpathian orogeny is the mountain-building event responsible for forming the Carpathian Mountains through the collision and deformation of tectonic plates in Central and Eastern Europe.
-
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.
Karelian orogeny
The Karelian orogeny was an ancient Paleoproterozoic mountain-building event that shaped much of the bedrock and geological structure of the Fennoscandian Shield in northern Europe.
-
E.
Pindus orogeny
The Pindus orogeny is a mountain-building event that formed much of the Pindus mountain range in Greece through the collision and deformation of tectonic plates during the Mesozoic–Cenozoic eras.
- F. None of above.
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Provenance (2 batches)
The batch behind each pipeline step, in order, with when it ran. Timestamps are batch-level — stages were processed in waves, so the object chain (NER → NED1 → NEDg → NED2) reads in order, but predicate / elicitation batches can sit in a different wave.
| Step | Stage | Batch ID | Status | When |
|---|---|---|---|---|
| creating | Elicitation | batch_69d8e514f2e08190ba70a4449519d218 |
completed | April 10, 2026, 11:55 a.m. |
| NER | Named-entity recognition | batch_69e6416e19d881909248c4f778f7147a |
completed | April 20, 2026, 3:08 p.m. |
Created at: April 10, 2026, 1:45 p.m.