Triple
T15200012
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Armorican Massif |
E363242
|
entity |
| Predicate | partOf |
P40
|
FINISHED |
| Object |
European Variscan Belt
The European Variscan Belt is a major Paleozoic mountain chain in western and central Europe formed by the collision of ancient continental plates during the Variscan orogeny.
|
E1144177
|
NE FINISHED |
How this triple was built (4 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: European Variscan Belt | Statement: [Armorican Massif, partOf, European Variscan Belt]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: European Variscan Belt Context triple: [Armorican Massif, partOf, European Variscan Belt]
-
A.
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.
-
B.
Moldanubian Zone
The Moldanubian Zone is a high-grade metamorphic and igneous core region of Central Europe, forming the oldest and most structurally complex part of the Bohemian Massif.
-
C.
Brunovistulian terrane
The Brunovistulian terrane is a Precambrian to early Paleozoic crustal block in Central Europe that forms part of the basement underlying the eastern Variscan orogen.
-
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.
East European Craton
The East European Craton is an ancient, stable part of the continental lithosphere underlying much of Eastern Europe, forming the geological core of regions such as Russia, Ukraine, and the Baltic states.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NEDg
Description generation
gpt-5.1
Instruction
Generate a one-sentence description of the target entity. You are given a context triple in the form (subject, predicate, object), where the object is the target entity. # Instructions Use the triple to infer relevant information about the entity. Describe the entity based on what is most defining, well-known. Avoid repeating the information from the triple, unless really essential. # Response Format Return only the sentence: "Description: [one-sentence description of the target entity]"
Input
Entity: European Variscan Belt Triple: [Armorican Massif, partOf, European Variscan Belt]
Generated description
The European Variscan Belt is a major Paleozoic mountain chain in western and central Europe formed by the collision of ancient continental plates during the Variscan orogeny.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: European Variscan Belt Target entity description: The European Variscan Belt is a major Paleozoic mountain chain in western and central Europe formed by the collision of ancient continental plates during the Variscan orogeny.
-
A.
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.
-
B.
Moldanubian Zone
The Moldanubian Zone is a high-grade metamorphic and igneous core region of Central Europe, forming the oldest and most structurally complex part of the Bohemian Massif.
-
C.
Brunovistulian terrane
The Brunovistulian terrane is a Precambrian to early Paleozoic crustal block in Central Europe that forms part of the basement underlying the eastern Variscan orogen.
-
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.
East European Craton
The East European Craton is an ancient, stable part of the continental lithosphere underlying much of Eastern Europe, forming the geological core of regions such as Russia, Ukraine, and the Baltic states.
- F. None of above. chosen
Provenance (5 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_69d85a0b78bc8190b6e5ad51a2c4cfc5 |
completed | April 10, 2026, 2:01 a.m. |
| NER | Named-entity recognition | batch_69e006b476208190a5119710c518bb1f |
completed | April 15, 2026, 9:44 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69fed3363f688190a5c728846bea743a |
completed | May 9, 2026, 6:24 a.m. |
| NEDg | Description generation | batch_69fed76d6a888190b44efa490df4b6d0 |
completed | May 9, 2026, 6:42 a.m. |
| NED2 | Entity disambiguation (via description) | batch_69feda443c64819087cb16ce742e7cc5 |
completed | May 9, 2026, 6:55 a.m. |
Created at: April 10, 2026, 3:10 a.m.