Triple
T23377826
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Makran subduction zone |
E593654
|
entity |
| Predicate | associatedWith |
P37
|
FINISHED |
| Object | Makran accretionary wedge |
—
|
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: Makran accretionary wedge | Statement: [Makran subduction zone, associatedWith, Makran accretionary wedge]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Makran accretionary wedge Context triple: [Makran subduction zone, associatedWith, Makran accretionary wedge]
-
A.
Makran subduction zone
The Makran subduction zone is a major convergent plate boundary in the northwestern Indian Ocean where the Arabian Plate is being subducted beneath the Eurasian Plate, capable of generating large earthquakes and tsunamis.
-
B.
Mediterranean Ridge accretionary complex
The Mediterranean Ridge accretionary complex is a vast submarine geological structure in the eastern Mediterranean formed by the ongoing convergence and subduction of tectonic plates, resulting in intense deformation and sediment accumulation.
-
C.
Franciscan subduction complex
The Franciscan subduction complex is a large, geologically complex assemblage of deformed and metamorphosed oceanic and continental margin rocks formed along the ancient subduction zone at the western edge of North America.
-
D.
Arabia–Eurasia collision zone
The Arabia–Eurasia collision zone is a major tectonic convergence region where the Arabian Plate is colliding with the Eurasian Plate, giving rise to extensive mountain building, seismic activity, and complex deformation across the Middle East and surrounding areas.
-
E.
Mediterranean back-arc domain
The Mediterranean back-arc domain is a tectonically active region behind the main plate convergence zones of the Mediterranean, characterized by extension, basin formation, and complex interactions between the African and Eurasian plates.
- 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: Makran accretionary wedge Target entity description: The Makran accretionary wedge is a large sedimentary complex formed by the scraping and stacking of oceanic sediments along the convergent plate boundary off the coasts of Iran and Pakistan.
-
A.
Makran subduction zone
chosen
The Makran subduction zone is a major convergent plate boundary in the northwestern Indian Ocean where the Arabian Plate is being subducted beneath the Eurasian Plate, capable of generating large earthquakes and tsunamis.
-
B.
Mediterranean Ridge accretionary complex
The Mediterranean Ridge accretionary complex is a vast submarine geological structure in the eastern Mediterranean formed by the ongoing convergence and subduction of tectonic plates, resulting in intense deformation and sediment accumulation.
-
C.
Franciscan subduction complex
The Franciscan subduction complex is a large, geologically complex assemblage of deformed and metamorphosed oceanic and continental margin rocks formed along the ancient subduction zone at the western edge of North America.
-
D.
Arabia–Eurasia collision zone
The Arabia–Eurasia collision zone is a major tectonic convergence region where the Arabian Plate is colliding with the Eurasian Plate, giving rise to extensive mountain building, seismic activity, and complex deformation across the Middle East and surrounding areas.
-
E.
Mediterranean back-arc domain
The Mediterranean back-arc domain is a tectonically active region behind the main plate convergence zones of the Mediterranean, characterized by extension, basin formation, and complex interactions between the African and Eurasian plates.
- F. None of above.
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_69e25d268a50819095f2fd479da8ef3f |
completed | April 17, 2026, 4:17 p.m. |
| NER | Named-entity recognition | batch_69f1a3b526ec8190b0304c72a9010abb |
completed | April 29, 2026, 6:22 a.m. |
Created at: April 17, 2026, 5:33 p.m.