Gulf of Aqaba pull-apart basins
E984279
UNEXPLORED
The Gulf of Aqaba pull-apart basins are a series of deep, elongated marine basins formed by strike-slip tectonics along the Dead Sea Transform fault at the northern end of the Red Sea.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Gulf of Aqaba pull-apart basins canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T12439871 — 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: Gulf of Aqaba pull-apart basins Context triple: [Dead Sea Transform fault, associatedFeature, Gulf of Aqaba pull-apart basins]
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A.
Tyrrhenian back-arc basin system
The Tyrrhenian back-arc basin system is a tectonically active region in the western Mediterranean characterized by seafloor spreading, extensional processes, and associated volcanic activity behind the Apennine subduction zone.
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B.
Aegean back-arc extension
Aegean back-arc extension is a tectonic process in the Aegean region characterized by crustal stretching and thinning behind the Hellenic subduction zone, leading to widespread normal faulting and basin formation.
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C.
Andean back-arc basins
Andean back-arc basins are sedimentary basins that formed behind the Andean volcanic arc due to tectonic extension and subsidence related to subduction along the western margin of South America.
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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.
Cayman Trough transform system
The Cayman Trough transform system is a major strike-slip plate boundary in the Caribbean region that accommodates relative motion between the North American and Caribbean tectonic plates.
- 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: Gulf of Aqaba pull-apart basins Target entity description: The Gulf of Aqaba pull-apart basins are a series of deep, elongated marine basins formed by strike-slip tectonics along the Dead Sea Transform fault at the northern end of the Red Sea.
-
A.
Tyrrhenian back-arc basin system
The Tyrrhenian back-arc basin system is a tectonically active region in the western Mediterranean characterized by seafloor spreading, extensional processes, and associated volcanic activity behind the Apennine subduction zone.
-
B.
Aegean back-arc extension
Aegean back-arc extension is a tectonic process in the Aegean region characterized by crustal stretching and thinning behind the Hellenic subduction zone, leading to widespread normal faulting and basin formation.
-
C.
Andean back-arc basins
Andean back-arc basins are sedimentary basins that formed behind the Andean volcanic arc due to tectonic extension and subsidence related to subduction along the western margin of South America.
-
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.
Cayman Trough transform system
The Cayman Trough transform system is a major strike-slip plate boundary in the Caribbean region that accommodates relative motion between the North American and Caribbean tectonic plates.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.