Triple
T15200013
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Armorican Massif |
E363242
|
entity |
| Predicate | partOf |
P40
|
FINISHED |
| Object |
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.
|
E1144178
|
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: West European Craton margin | Statement: [Armorican Massif, partOf, West European Craton margin]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: West European Craton margin Context triple: [Armorican Massif, partOf, West European Craton margin]
-
A.
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.
-
B.
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.
-
C.
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.
-
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.
Australia craton (in many models)
Australia craton (in many models) is an ancient, stable piece of continental lithosphere that is often reconstructed as a major component of the supercontinent Rodinia in Precambrian tectonic models.
- 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: West European Craton margin Triple: [Armorican Massif, partOf, West European Craton margin]
Generated description
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.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: West European Craton margin Target entity description: 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.
-
A.
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.
-
B.
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.
-
C.
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.
-
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.
Australia craton (in many models)
Australia craton (in many models) is an ancient, stable piece of continental lithosphere that is often reconstructed as a major component of the supercontinent Rodinia in Precambrian tectonic models.
- 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.