Triple
T9143246
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | North China Craton |
E219383
|
entity |
| Predicate | hasSubdivision |
P747
|
FINISHED |
| Object |
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.
|
E781049
|
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: Trans-North China Orogen | Statement: [North China Craton, hasSubdivision, Trans-North China Orogen]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Trans-North China Orogen Context triple: [North China Craton, hasSubdivision, Trans-North China Orogen]
-
A.
North China Craton
The North China Craton is an ancient, once-stable block of continental crust in northern China that preserves some of Earth’s oldest rocks and records a complex history of tectonic assembly and destruction.
-
B.
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.
-
C.
Yanshanian orogeny
The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
-
D.
South China Block
The South China Block is a major continental tectonic block in East Asia that underlies much of southern China and adjacent regions, playing a key role in the geological evolution of the western Pacific margin.
-
E.
Chinese continental crust
The Chinese continental crust is the extensive, geologically complex portion of Earth’s crust underlying much of China, composed of multiple ancient tectonic blocks and plates that have amalgamated over hundreds of millions of years.
- 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: Trans-North China Orogen Triple: [North China Craton, hasSubdivision, Trans-North China Orogen]
Generated description
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.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Trans-North China Orogen Target entity description: 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.
-
A.
North China Craton
The North China Craton is an ancient, once-stable block of continental crust in northern China that preserves some of Earth’s oldest rocks and records a complex history of tectonic assembly and destruction.
-
B.
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.
-
C.
Yanshanian orogeny
The Yanshanian orogeny was a major Mesozoic mountain-building event in northern China that significantly reshaped the geology and structure of the Yan Mountains and surrounding regions.
-
D.
South China Block
The South China Block is a major continental tectonic block in East Asia that underlies much of southern China and adjacent regions, playing a key role in the geological evolution of the western Pacific margin.
-
E.
Chinese continental crust
The Chinese continental crust is the extensive, geologically complex portion of Earth’s crust underlying much of China, composed of multiple ancient tectonic blocks and plates that have amalgamated over hundreds of millions of years.
- F. None of above. chosen
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_69ca83e121dc81909912bd66953081c5 |
completed | March 30, 2026, 2:08 p.m. |
| NER | Named-entity recognition | batch_69cca8f5f740819098236ada5b95889d |
completed | April 1, 2026, 5:11 a.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69d048186cc88190be4f515c16c20450 |
completed | April 3, 2026, 11:07 p.m. |
| NEDg | Description generation | batch_69d0496672a881909c1ac91a7ec1a2a1 |
completed | April 3, 2026, 11:12 p.m. |
| NED2 | Entity disambiguation (via description) | batch_69d04a35451881909dfe6795b743b026 |
completed | April 3, 2026, 11:16 p.m. |
Created at: March 30, 2026, 7:19 p.m.