Triple
T11785030
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Karakoram orogeny |
E280248
|
entity |
| Predicate | associatedWith |
P37
|
FINISHED |
| Object |
Karakoram fault system
The Karakoram fault system is a major strike-slip fault zone in the western Himalaya–Tibetan region that accommodates significant tectonic movement and has played a key role in shaping the high-relief Karakoram and adjacent mountain ranges.
|
E946368
|
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: Karakoram fault system | Statement: [Karakoram orogeny, associatedWith, Karakoram fault system]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Karakoram fault system Context triple: [Karakoram orogeny, associatedWith, Karakoram fault system]
-
A.
Altyn Tagh Fault
The Altyn Tagh Fault is a major strike-slip fault system in northwestern China that plays a key role in accommodating the tectonic deformation of the Tibetan Plateau.
-
B.
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.
-
C.
Karakoram glacial system
The Karakoram glacial system is an extensive network of high-altitude glaciers in the Karakoram Range, notable for its large ice masses, complex glacier dynamics, and significant influence on regional water resources.
-
D.
Himalayan Frontal Thrust
The Himalayan Frontal Thrust is the youngest and most active major fault system along the southern front of the Himalayas, accommodating much of the ongoing convergence between the Indian and Eurasian tectonic plates.
-
E.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
- 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: Karakoram fault system Triple: [Karakoram orogeny, associatedWith, Karakoram fault system]
Generated description
The Karakoram fault system is a major strike-slip fault zone in the western Himalaya–Tibetan region that accommodates significant tectonic movement and has played a key role in shaping the high-relief Karakoram and adjacent mountain ranges.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Karakoram fault system Target entity description: The Karakoram fault system is a major strike-slip fault zone in the western Himalaya–Tibetan region that accommodates significant tectonic movement and has played a key role in shaping the high-relief Karakoram and adjacent mountain ranges.
-
A.
Altyn Tagh Fault
The Altyn Tagh Fault is a major strike-slip fault system in northwestern China that plays a key role in accommodating the tectonic deformation of the Tibetan Plateau.
-
B.
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.
-
C.
Karakoram glacial system
The Karakoram glacial system is an extensive network of high-altitude glaciers in the Karakoram Range, notable for its large ice masses, complex glacier dynamics, and significant influence on regional water resources.
-
D.
Himalayan Frontal Thrust
The Himalayan Frontal Thrust is the youngest and most active major fault system along the southern front of the Himalayas, accommodating much of the ongoing convergence between the Indian and Eurasian tectonic plates.
-
E.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
- 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_69d6ab258b808190b1735835c841e3a4 |
completed | April 8, 2026, 7:23 p.m. |
| NER | Named-entity recognition | batch_69d8a585795c8190aa8a5edf0d99b47f |
completed | April 10, 2026, 7:23 a.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69f090d861f481909b920197a3d60e28 |
completed | April 28, 2026, 10:50 a.m. |
| NEDg | Description generation | batch_69f0bd3f39608190b29027b30664bd9c |
completed | April 28, 2026, 1:59 p.m. |
| NED2 | Entity disambiguation (via description) | batch_69f0ef5afd448190953b5d9929478132 |
completed | April 28, 2026, 5:33 p.m. |
Created at: April 8, 2026, 9:42 p.m.