Triple
T22821173
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Delaware Basin |
E565232
|
entity |
| Predicate | partOf |
P40
|
FINISHED |
| Object | North American craton margin |
—
|
NE NERFINISHED |
How this triple was built (3 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: North American craton margin | Statement: [Delaware Basin, partOf, North American craton margin]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: North American craton margin Context triple: [Delaware Basin, partOf, North American craton margin]
-
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.
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.
-
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.
North Atlantic rifted margin system
The North Atlantic rifted margin system is a vast geological province formed by the breakup of the supercontinent Pangaea and the opening of the North Atlantic Ocean, characterized by extensive passive continental margins, sedimentary basins, and volcanic features along the ocean’s edges.
-
E.
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.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: North American craton margin Target entity description: The North American craton margin is the tectonic boundary zone where the stable ancient core of the North American continent transitions into younger, more deformed geological provinces and sedimentary basins.
-
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.
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.
-
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.
North Atlantic rifted margin system
The North Atlantic rifted margin system is a vast geological province formed by the breakup of the supercontinent Pangaea and the opening of the North Atlantic Ocean, characterized by extensive passive continental margins, sedimentary basins, and volcanic features along the ocean’s edges.
-
E.
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.
- F. None of above. chosen
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_69e2458426188190b58b8ab4844fe420 |
completed | April 17, 2026, 2:36 p.m. |
| NER | Named-entity recognition | batch_69f17dcffdd88190a5f9c780c71b5053 |
completed | April 29, 2026, 3:41 a.m. |
Created at: April 17, 2026, 3:33 p.m.