Triple
T20273705
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Vøring Margin |
E502956
|
entity |
| Predicate | partOf |
P40
|
FINISHED |
| Object | North Atlantic rifted margin system |
—
|
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 Atlantic rifted margin system | Statement: [Vøring Margin, partOf, North Atlantic rifted margin system]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: North Atlantic rifted margin system Context triple: [Vøring Margin, partOf, North Atlantic rifted margin system]
-
A.
North Sea rift system
The North Sea rift system is a major geological rift complex underlying the North Sea, formed by extensive Mesozoic and Cenozoic crustal extension that created numerous sedimentary basins important for hydrocarbon resources.
-
B.
North Atlantic fracture zone system
The North Atlantic fracture zone system is a network of major oceanic crustal faults and offsets that segment the Mid-Atlantic Ridge and shape the seafloor topography of the North Atlantic Ocean.
-
C.
Southwest Indian Ocean passive margin system
The Southwest Indian Ocean passive margin system is a broad tectonic and sedimentary region along the western Indian Ocean where the continental crust of Madagascar and nearby areas transitions into oceanic crust formed during the breakup of Gondwana.
-
D.
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.
-
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 Atlantic rifted margin system Target entity description: 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.
-
A.
North Sea rift system
The North Sea rift system is a major geological rift complex underlying the North Sea, formed by extensive Mesozoic and Cenozoic crustal extension that created numerous sedimentary basins important for hydrocarbon resources.
-
B.
North Atlantic fracture zone system
The North Atlantic fracture zone system is a network of major oceanic crustal faults and offsets that segment the Mid-Atlantic Ridge and shape the seafloor topography of the North Atlantic Ocean.
-
C.
Southwest Indian Ocean passive margin system
The Southwest Indian Ocean passive margin system is a broad tectonic and sedimentary region along the western Indian Ocean where the continental crust of Madagascar and nearby areas transitions into oceanic crust formed during the breakup of Gondwana.
-
D.
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.
-
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_69e0b4b0e79c8190bd61f22ef1329fa8 |
completed | April 16, 2026, 10:06 a.m. |
| NER | Named-entity recognition | batch_69e675e104f081909d17c1963a5db528 |
completed | April 20, 2026, 6:52 p.m. |
Created at: April 16, 2026, 10:28 a.m.