Triple

T16634915
Position Surface form Disambiguated ID Type / Status
Subject Qinling–Dabie orogeny E404173 entity
Predicate relatedTo P37 FINISHED
Object Qinling–Dabie–Sulu orogenic belt
The Qinling–Dabie–Sulu orogenic belt is a major east–west-trending mountain and suture zone in central-eastern China formed by the collision of the North China and South China blocks, notable for its high- and ultrahigh-pressure metamorphic rocks.
E404173 NE FINISHED

How this triple was built (4 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: Qinling–Dabie–Sulu orogenic belt | Statement: [Qinling–Dabie orogeny, relatedTo, Qinling–Dabie–Sulu orogenic belt]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07
Target entity: Qinling–Dabie–Sulu orogenic belt
Context triple: [Qinling–Dabie orogeny, relatedTo, Qinling–Dabie–Sulu orogenic belt]
  • A. Qinling–Dabie orogeny
    The Qinling–Dabie orogeny was a major Paleozoic–Mesozoic mountain-building event in central China that formed the Qinling and Dabie mountain ranges through the collision of the North China and South China tectonic blocks.
  • B. Central Asian Orogenic Belt
    The Central Asian Orogenic Belt is a vast, geologically complex mountain-building region in Eurasia formed by the long-term collision and accretion of multiple continental and oceanic terranes.
  • C. Trans-North China Orogen
    The Trans-North China Orogen is a major Paleoproterozoic collisional belt in northern China that records the suturing of ancient continental blocks within the North China Craton.
  • D. Jiangnan orogen
    The Jiangnan orogen is a major Precambrian mountain-building belt in southern China formed by the collision and amalgamation of ancient continental blocks.
  • E. Songpan–Ganzi terrane
    The Songpan–Ganzi terrane is a geologically complex region in eastern Tibet characterized by thick Triassic sedimentary sequences and intense deformation associated with the growth of the Tibetan Plateau.
  • F. None of above. chosen
  • G. Unsure - the case is ambiguous/there is not enough information to decide.
NEDg Description generation gpt-5.1
Instruction
Generate a one-sentence description of the target entity. 
You are given a context triple in the form (subject, predicate, object), where the object is the target entity. 
# Instructions
Use the triple to infer relevant information about the entity. Describe the entity based on what is most defining, well-known. 
Avoid repeating the information from the triple, unless really essential.
# Response Format
Return only the sentence: "Description: [one-sentence description of the target entity]"
Input
Entity: Qinling–Dabie–Sulu orogenic belt
Triple: [Qinling–Dabie orogeny, relatedTo, Qinling–Dabie–Sulu orogenic belt]
Generated description
The Qinling–Dabie–Sulu orogenic belt is a major east–west-trending mountain and suture zone in central-eastern China formed by the collision of the North China and South China blocks, notable for its high- and ultrahigh-pressure metamorphic rocks.
NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07
Target entity: Qinling–Dabie–Sulu orogenic belt
Target entity description: The Qinling–Dabie–Sulu orogenic belt is a major east–west-trending mountain and suture zone in central-eastern China formed by the collision of the North China and South China blocks, notable for its high- and ultrahigh-pressure metamorphic rocks.
  • A. Qinling–Dabie orogeny chosen
    The Qinling–Dabie orogeny was a major Paleozoic–Mesozoic mountain-building event in central China that formed the Qinling and Dabie mountain ranges through the collision of the North China and South China tectonic blocks.
  • B. Central Asian Orogenic Belt
    The Central Asian Orogenic Belt is a vast, geologically complex mountain-building region in Eurasia formed by the long-term collision and accretion of multiple continental and oceanic terranes.
  • C. Trans-North China Orogen
    The Trans-North China Orogen is a major Paleoproterozoic collisional belt in northern China that records the suturing of ancient continental blocks within the North China Craton.
  • D. Jiangnan orogen
    The Jiangnan orogen is a major Precambrian mountain-building belt in southern China formed by the collision and amalgamation of ancient continental blocks.
  • E. Songpan–Ganzi terrane
    The Songpan–Ganzi terrane is a geologically complex region in eastern Tibet characterized by thick Triassic sedimentary sequences and intense deformation associated with the growth of the Tibetan Plateau.
  • F. None of above.

Provenance (5 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_69d8838a41f08190b0c3f79c47df5078 completed April 10, 2026, 4:58 a.m.
NER Named-entity recognition batch_69e378e8a76c8190bf08e6f6dec63c50 completed April 18, 2026, 12:28 p.m.
NED1 Entity disambiguation (via context triple) batch_6a008a2b3a608190ad8d2b653cd8785d completed May 10, 2026, 1:37 p.m.
NEDg Description generation batch_6a008b001c988190b0ddec3be0ed6fd0 completed May 10, 2026, 1:41 p.m.
NED2 Entity disambiguation (via description) batch_6a008ba8227881908b1ac6e30d2e7c32 completed May 10, 2026, 1:44 p.m.
Created at: April 10, 2026, 5:17 a.m.