Mediterranean back-arc domain
E1543342
UNEXPLORED
The Mediterranean back-arc domain is a tectonically active region behind the main plate convergence zones of the Mediterranean, characterized by extension, basin formation, and complex interactions between the African and Eurasian plates.
All labels observed (3)
| Label | Occurrences |
|---|---|
| Mediterranean back-arc and rift systems | 1 |
| Mediterranean back-arc basin system | 1 |
| Mediterranean back-arc domain canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T22553661 — 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: Mediterranean back-arc domain Context triple: [Tyrrhenian back-arc basin system, partOf, Mediterranean back-arc domain]
-
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.
Mediterranean Ridge accretionary complex
The Mediterranean Ridge accretionary complex is a vast submarine geological structure in the eastern Mediterranean formed by the ongoing convergence and subduction of tectonic plates, resulting in intense deformation and sediment accumulation.
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D.
Cascadia back-arc region
The Cascadia back-arc region is a tectonically active area east of the Cascadia subduction zone characterized by crustal extension, volcanism, and associated magmatic and geothermal activity.
-
E.
Mediterranean volcanic province
The Mediterranean volcanic province is a geologically active region surrounding the Mediterranean Sea, characterized by numerous volcanic arcs, islands, and complexes formed by complex plate interactions and subduction processes.
- 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: Mediterranean back-arc domain Target entity description: The Mediterranean back-arc domain is a tectonically active region behind the main plate convergence zones of the Mediterranean, characterized by extension, basin formation, and complex interactions between the African and Eurasian plates.
-
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.
Mediterranean Ridge accretionary complex
The Mediterranean Ridge accretionary complex is a vast submarine geological structure in the eastern Mediterranean formed by the ongoing convergence and subduction of tectonic plates, resulting in intense deformation and sediment accumulation.
-
D.
Cascadia back-arc region
The Cascadia back-arc region is a tectonically active area east of the Cascadia subduction zone characterized by crustal extension, volcanism, and associated magmatic and geothermal activity.
-
E.
Mediterranean volcanic province
The Mediterranean volcanic province is a geologically active region surrounding the Mediterranean Sea, characterized by numerous volcanic arcs, islands, and complexes formed by complex plate interactions and subduction processes.
- F. None of above. chosen
Referenced by (3)
Full triples — surface form annotated when it differs from this entity's canonical label.
linked to: Mediterranean back-arc domain
linked to: Mediterranean back-arc domain