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.