Triple
T4648353
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Pan-African orogeny |
E102227
|
entity |
| Predicate | linkedTo |
P37
|
FINISHED |
| Object |
Brasiliano–Pan-African orogenic system
The Brasiliano–Pan-African orogenic system is a vast Neoproterozoic mountain-building belt that records the assembly of the Gondwana supercontinent through the collision and suturing of multiple continental blocks across what are now South America, Africa, and adjacent regions.
|
E102227
|
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: Brasiliano–Pan-African orogenic system | Statement: [Pan-African orogeny, linkedTo, Brasiliano–Pan-African orogenic system]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Brasiliano–Pan-African orogenic system Context triple: [Pan-African orogeny, linkedTo, Brasiliano–Pan-African orogenic system]
-
A.
Pan-African orogeny
The Pan-African orogeny was a widespread Neoproterozoic mountain-building event that assembled parts of the supercontinent Gondwana across Africa and adjoining regions.
-
B.
Guiana Shield
The Guiana Shield is a geologically ancient, mineral-rich craton in northern South America, characterized by extensive tropical rainforests, unique biodiversity, and dramatic table-top mountains.
-
C.
Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
-
D.
West African Craton
The West African Craton is an ancient, stable block of continental crust in West Africa that forms a core part of the Precambrian geology of the African continent.
-
E.
Kalahari Craton
The Kalahari Craton is an ancient, stable block of continental crust underlying much of southern Africa and forming a key component of Earth’s early Precambrian geology.
- 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: Brasiliano–Pan-African orogenic system Triple: [Pan-African orogeny, linkedTo, Brasiliano–Pan-African orogenic system]
Generated description
The Brasiliano–Pan-African orogenic system is a vast Neoproterozoic mountain-building belt that records the assembly of the Gondwana supercontinent through the collision and suturing of multiple continental blocks across what are now South America, Africa, and adjacent regions.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Brasiliano–Pan-African orogenic system Target entity description: The Brasiliano–Pan-African orogenic system is a vast Neoproterozoic mountain-building belt that records the assembly of the Gondwana supercontinent through the collision and suturing of multiple continental blocks across what are now South America, Africa, and adjacent regions.
-
A.
Pan-African orogeny
chosen
The Pan-African orogeny was a widespread Neoproterozoic mountain-building event that assembled parts of the supercontinent Gondwana across Africa and adjoining regions.
-
B.
Guiana Shield
The Guiana Shield is a geologically ancient, mineral-rich craton in northern South America, characterized by extensive tropical rainforests, unique biodiversity, and dramatic table-top mountains.
-
C.
Cadomian orogeny
The Cadomian orogeny was a late Neoproterozoic mountain-building event that shaped parts of what are now western Europe, contributing to the assembly of the supercontinent Pannotia.
-
D.
West African Craton
The West African Craton is an ancient, stable block of continental crust in West Africa that forms a core part of the Precambrian geology of the African continent.
-
E.
Kalahari Craton
The Kalahari Craton is an ancient, stable block of continental crust underlying much of southern Africa and forming a key component of Earth’s early Precambrian geology.
- 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_69bd43d71a308190afea7280841b0de8 |
completed | March 20, 2026, 12:55 p.m. |
| NER | Named-entity recognition | batch_69bd62feeb6c8190a7807c37e9a6fa00 |
completed | March 20, 2026, 3:08 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69bdfae3d8f4819082ec002bc4d9819d |
completed | March 21, 2026, 1:56 a.m. |
| NEDg | Description generation | batch_69bdfba6f8e08190ad6c802ec1cb5ce2 |
completed | March 21, 2026, 2 a.m. |
| NED2 | Entity disambiguation (via description) | batch_69bdfc6ac91c819090776365d3dc05d4 |
completed | March 21, 2026, 2:03 a.m. |
Created at: March 20, 2026, 1:14 p.m.