Triple
T21028103
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Xining Basin |
E517992
|
entity |
| Predicate | partOf |
P40
|
FINISHED |
| Object | Tibetan Plateau foreland basins |
—
|
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: Tibetan Plateau foreland basins | Statement: [Xining Basin, partOf, Tibetan Plateau foreland basins]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Tibetan Plateau foreland basins Context triple: [Xining Basin, partOf, Tibetan Plateau foreland basins]
-
A.
Himalayan foreland basin
The Himalayan foreland basin is a vast sedimentary basin formed along the southern margin of the rising Himalayas, where eroded material from the mountain range accumulates before being transported further afield.
-
B.
Caledonian foreland basins
Caledonian foreland basins are a group of sedimentary basins that developed in front of the Caledonian orogenic belt during Paleozoic mountain-building in what is now parts of northern Europe, including areas such as the Orcadian Basin.
-
C.
South Tibetan Detachment System
The South Tibetan Detachment System is a major normal fault system in the Himalaya that accommodated crustal extension and exhumation of high-grade metamorphic rocks above the Main Central Thrust.
-
D.
Indian Gondwana basins
The Indian Gondwana basins are a series of continental sedimentary basins in peninsular India renowned for their extensive Permian–Mesozoic coal-bearing strata, fossil assemblages, and insights into the geological evolution of the ancient supercontinent Gondwana.
-
E.
Laramide foreland basin
The Laramide foreland basin is a broad sedimentary basin that formed east of the rising Rocky Mountains during the Late Cretaceous to early Paleogene Laramide orogeny, accumulating thick sequences of continental and marine deposits.
- 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: Tibetan Plateau foreland basins Target entity description: Tibetan Plateau foreland basins are a series of sedimentary basins surrounding the margins of the Tibetan Plateau that record its uplift, deformation, and associated climatic and erosional history.
-
A.
Himalayan foreland basin
The Himalayan foreland basin is a vast sedimentary basin formed along the southern margin of the rising Himalayas, where eroded material from the mountain range accumulates before being transported further afield.
-
B.
Caledonian foreland basins
Caledonian foreland basins are a group of sedimentary basins that developed in front of the Caledonian orogenic belt during Paleozoic mountain-building in what is now parts of northern Europe, including areas such as the Orcadian Basin.
-
C.
South Tibetan Detachment System
The South Tibetan Detachment System is a major normal fault system in the Himalaya that accommodated crustal extension and exhumation of high-grade metamorphic rocks above the Main Central Thrust.
-
D.
Indian Gondwana basins
The Indian Gondwana basins are a series of continental sedimentary basins in peninsular India renowned for their extensive Permian–Mesozoic coal-bearing strata, fossil assemblages, and insights into the geological evolution of the ancient supercontinent Gondwana.
-
E.
Laramide foreland basin
The Laramide foreland basin is a broad sedimentary basin that formed east of the rising Rocky Mountains during the Late Cretaceous to early Paleogene Laramide orogeny, accumulating thick sequences of continental and marine deposits.
- 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_69e0b503275c8190afd9a163f997c709 |
completed | April 16, 2026, 10:08 a.m. |
| NER | Named-entity recognition | batch_69e6fc7efda081909a4de1c389166bf2 |
completed | April 21, 2026, 4:26 a.m. |
Created at: April 16, 2026, 1:55 p.m.