Paleozoic succession of the Amadeus Basin
E973666
UNEXPLORED
The Paleozoic succession of the Amadeus Basin is a thick, long-lived sedimentary sequence in central Australia that records marine and terrestrial environments from the early Paleozoic through to the late Paleozoic within an intracratonic basin setting.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Paleozoic succession of the Amadeus Basin canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T12320050 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Paleozoic succession of the Amadeus Basin Context triple: [Hermannsburg Sandstone, stratigraphicUnitOf, Paleozoic succession of the Amadeus Basin]
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A.
Indian Gondwana basins
The Indian Gondwana basins are a series of continental sedimentary basins in peninsular India renowned for their extensive Permian–Mesozoic coal-bearing strata, fossil assemblages, and insights into the geological evolution of the ancient supercontinent Gondwana.
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B.
Magnesian Limestone succession
The Magnesian Limestone succession is a geological sequence of Permian-age dolomitic limestone formations that forms a distinctive belt across parts of northern and central England.
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C.
Djadokhta Formation
The Djadokhta Formation is a Late Cretaceous sedimentary rock unit in Mongolia renowned for its exceptionally well-preserved dinosaur fossils, including iconic theropods and other desert-adapted fauna.
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D.
Caledonian foreland basins
Caledonian foreland basins are a group of sedimentary basins that developed in front of the Caledonian orogenic belt during Paleozoic mountain-building in what is now parts of northern Europe, including areas such as the Orcadian Basin.
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E.
Emu Bay Shale
Emu Bay Shale is a renowned Cambrian fossil deposit in South Australia noted for its exceptionally well-preserved soft-bodied marine organisms.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Paleozoic succession of the Amadeus Basin Target entity description: The Paleozoic succession of the Amadeus Basin is a thick, long-lived sedimentary sequence in central Australia that records marine and terrestrial environments from the early Paleozoic through to the late Paleozoic within an intracratonic basin setting.
-
A.
Indian Gondwana basins
The Indian Gondwana basins are a series of continental sedimentary basins in peninsular India renowned for their extensive Permian–Mesozoic coal-bearing strata, fossil assemblages, and insights into the geological evolution of the ancient supercontinent Gondwana.
-
B.
Magnesian Limestone succession
The Magnesian Limestone succession is a geological sequence of Permian-age dolomitic limestone formations that forms a distinctive belt across parts of northern and central England.
-
C.
Djadokhta Formation
The Djadokhta Formation is a Late Cretaceous sedimentary rock unit in Mongolia renowned for its exceptionally well-preserved dinosaur fossils, including iconic theropods and other desert-adapted fauna.
-
D.
Caledonian foreland basins
Caledonian foreland basins are a group of sedimentary basins that developed in front of the Caledonian orogenic belt during Paleozoic mountain-building in what is now parts of northern Europe, including areas such as the Orcadian Basin.
-
E.
Emu Bay Shale
Emu Bay Shale is a renowned Cambrian fossil deposit in South Australia noted for its exceptionally well-preserved soft-bodied marine organisms.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.