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.