Triple

T19725888
Position Surface form Disambiguated ID Type / Status
Subject Baikal orogeny E473725 entity
Predicate affects P9 FINISHED
Object 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.
E1392858 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: Siberian craton margins | Statement: [Baikal orogeny, affects, Siberian craton margins]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07
Target entity: Siberian craton margins
Context triple: [Baikal orogeny, affects, Siberian craton margins]
  • A. 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.
  • 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. East Antarctic craton basement
    The East Antarctic craton basement is an ancient, stable block of continental crust underlying much of East Antarctica, forming a key part of the continent’s geological core.
  • D. Panthalassa Ocean margins
    The Panthalassa Ocean margins were the extensive continental and volcanic arc boundaries of the vast Panthalassa superocean that surrounded the supercontinent Pangaea during much of the Mesozoic Era.
  • E. Western Block of the North China Craton
    The Western Block of the North China Craton is an ancient Archean to Paleoproterozoic continental crustal segment forming the western part of the North China Craton, notable for its old metamorphic basement and complex tectonic history.
  • 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: Siberian craton margins
Triple: [Baikal orogeny, affects, Siberian craton margins]
Generated description
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.
NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07
Target entity: Siberian craton margins
Target entity description: 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.
  • A. 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.
  • 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. East Antarctic craton basement
    The East Antarctic craton basement is an ancient, stable block of continental crust underlying much of East Antarctica, forming a key part of the continent’s geological core.
  • D. Panthalassa Ocean margins
    The Panthalassa Ocean margins were the extensive continental and volcanic arc boundaries of the vast Panthalassa superocean that surrounded the supercontinent Pangaea during much of the Mesozoic Era.
  • E. Western Block of the North China Craton
    The Western Block of the North China Craton is an ancient Archean to Paleoproterozoic continental crustal segment forming the western part of the North China Craton, notable for its old metamorphic basement and complex tectonic history.
  • 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_69d8e517ebd48190979ee76723bcfadf completed April 10, 2026, 11:55 a.m.
NER Named-entity recognition batch_69e649f7bedc81908f784832c0fc10a1 completed April 20, 2026, 3:44 p.m.
NED1 Entity disambiguation (via context triple) batch_6a07b4ee6b24819080a73814f45b76b3 completed May 16, 2026, 12:06 a.m.
NEDg Description generation batch_6a07b5e9961881908f224154ec12c366 completed May 16, 2026, 12:10 a.m.
NED2 Entity disambiguation (via description) batch_6a07b67964b481909af269c6b5db6527 completed May 16, 2026, 12:12 a.m.
Created at: April 10, 2026, 1:46 p.m.