Triple

T21807658
Position Surface form Disambiguated ID Type / Status
Subject Svecofennian orogeny E538388 entity
Predicate precededBy P97 FINISHED
Object Karelia–Norrbotten crustal evolution events 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: Karelia–Norrbotten crustal evolution events | Statement: [Svecofennian orogeny, precededBy, Karelia–Norrbotten crustal evolution events]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07
Target entity: Karelia–Norrbotten crustal evolution events
Context triple: [Svecofennian orogeny, precededBy, Karelia–Norrbotten crustal evolution events]
  • A. Siberian craton margins
    The Siberian craton margins are the ancient, stable outer zones of the Siberian continental core that were tectonically deformed and reworked during major mountain-building events such as the Baikal orogeny.
  • B. Midcontinent Granite-Rhyolite Province margins
    The Midcontinent Granite-Rhyolite Province margins are ancient crustal boundaries in the central United States that record tectonic and magmatic activity associated with the Proterozoic assembly of North America.
  • C. Karelian orogeny chosen
    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.
  • D. West European Craton margin
    The West European Craton margin is the ancient, stable geological boundary zone of the West European Craton, marking the transition between its old continental core and surrounding younger tectonic regions.
  • E. European Cenozoic Rift System
    The European Cenozoic Rift System is a major network of tectonic rift valleys and basins that formed across western and central Europe during the Cenozoic era, significantly shaping the region’s topography and volcanic activity.
  • 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_69e0c473f0f8819086c9d1b4a143bd67 completed April 16, 2026, 11:13 a.m.
NER Named-entity recognition batch_69f078047ca88190a0efa4bc7f2faf80 completed April 28, 2026, 9:04 a.m.
Created at: April 16, 2026, 6:53 p.m.