Triple

T880413
Position Surface form Disambiguated ID Type / Status
Subject Lesser Caucasus E19012 entity
Predicate orogeny P946 FINISHED
Object Alpine orogeny E102476 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: Alpine orogeny | Statement: [Lesser Caucasus, orogeny, Alpine orogeny]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07 
Target entity: Alpine orogeny
Context triple: [Lesser Caucasus, orogeny, Alpine orogeny]
  • A. Alpine orogeny chosen
    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.
  • B. Himalayan orogeny
    The Himalayan orogeny is the major mountain-building event resulting from the collision of the Indian and Eurasian tectonic plates, responsible for creating the Himalayan mountain range and the Tibetan Plateau.
  • C. 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.
  • D. Taconic orogeny
    The Taconic orogeny was an early Paleozoic mountain-building event along the eastern margin of ancient North America that contributed significantly to the formation of the Appalachian Mountains.
  • E. 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.
  • 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_69a4939c32488190a7ccd41cf0abb22b completed March 1, 2026, 7:29 p.m.
NER Named-entity recognition batch_69a4accb653c81909fe0753f78145be9 completed March 1, 2026, 9:16 p.m.
NED1 Entity disambiguation (via context triple) batch_69a7ee0053d88190be8705b42d172ab7 completed March 4, 2026, 8:32 a.m.
Created at: March 1, 2026, 7:39 p.m.