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.