Triple
T7615411
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Alpine-Carpathian mountain system |
E172348
|
entity |
| Predicate | relatedTo |
P37
|
FINISHED |
| Object | Mediterranean-Alpine orogenic system |
E32406
|
NE FINISHED |
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: Mediterranean-Alpine orogenic system | Statement: [Alpine-Carpathian mountain system, relatedTo, Mediterranean-Alpine orogenic system]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Mediterranean-Alpine orogenic system Context triple: [Alpine-Carpathian mountain system, relatedTo, Mediterranean-Alpine orogenic system]
-
A.
Alpine-Himalayan orogenic belt
chosen
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
-
B.
Alpine orogeny
The Alpine orogeny is a major mountain-building event that created the Alps and other ranges across southern Europe and parts of Asia through the collision of tectonic plates during the Cenozoic Era.
-
C.
Apennine orogeny
The Apennine orogeny is the mountain-building event responsible for forming Italy’s Apennine Mountains through the collision and complex interaction of the African and Eurasian tectonic plates.
-
D.
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.
-
E.
Scandinavian Caledonides
The Scandinavian Caledonides are a major Paleozoic mountain belt in Scandinavia formed by the collision of ancient continental plates during the Caledonian orogeny.
- F. None of above.
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Provenance (3 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_69c6994f50808190ba228764bb422417 |
completed | March 27, 2026, 2:50 p.m. |
| NER | Named-entity recognition | batch_69c6fa4392e881908ed1ab3f64b41600 |
completed | March 27, 2026, 9:44 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69c8686d16808190bc431c43c0928f6e |
completed | March 28, 2026, 11:46 p.m. |
Created at: March 27, 2026, 3:55 p.m.