Triple
T9143182
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Siberian Craton |
E219382
|
entity |
| Predicate | boundedBy |
P224
|
FINISHED |
| Object |
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.
|
E781044
|
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: Central Asian Orogenic Belt | Statement: [Siberian Craton, boundedBy, Central Asian Orogenic Belt]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Central Asian Orogenic Belt Context triple: [Siberian Craton, boundedBy, Central Asian Orogenic Belt]
-
A.
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.
-
B.
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.
-
C.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
-
D.
Indus-Tsangpo Suture Zone
The Indus-Tsangpo Suture Zone is a major tectonic boundary in the Himalayas marking the collision zone between the Indian and Eurasian plates, where remnants of the ancient Tethys Ocean crust are preserved.
-
E.
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.
- 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: Central Asian Orogenic Belt Triple: [Siberian Craton, boundedBy, Central Asian Orogenic Belt]
Generated description
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.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Central Asian Orogenic Belt Target entity description: 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.
-
A.
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.
-
B.
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.
-
C.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
-
D.
Indus-Tsangpo Suture Zone
The Indus-Tsangpo Suture Zone is a major tectonic boundary in the Himalayas marking the collision zone between the Indian and Eurasian plates, where remnants of the ancient Tethys Ocean crust are preserved.
-
E.
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.
- 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.