New Hebrides back-arc basin

E736668

The New Hebrides back-arc basin is a seafloor spreading region in the southwest Pacific formed behind the New Hebrides island arc as a result of subduction-related tectonic extension.

All labels observed (3)

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf back-arc basin
geological feature
seafloor spreading center
associatedWith New Hebrides subduction zone
Vanuatu island arc
developedBehind New Hebrides volcanic arc
formedBy subduction-related tectonic extension
geologicalOrigin subduction-driven extension
hasFeature extensional faulting
oceanic crust
spreading ridges
hasProcess crustal extension
seafloor spreading
hasRelevanceTo arc volcanism
earthquake activity in Vanuatu region
subduction dynamics
hasTectonicRegime extensional
transtensional
isPartOf New Hebrides arc-back-arc system
isStudiedIn geophysics
marine geology
plate tectonics
isTypeOf ocean basin
locatedBehind New Hebrides island arc
locatedIn Pacific Ocean
southwest Pacific Ocean
partOf southwest Pacific back-arc system
relatedTo convergence between Australian Plate and Pacific Plate
subduction of the Australian Plate
tectonicSetting back-arc region

How these facts were elicited

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

New Hebrides Trench isAdjacentTo New Hebrides back-arc basin
New Hebrides back-arc basin isPartOf New Hebrides arc-back-arc system
linked to: New Hebrides back-arc basin
Norfolk Basin partOf Southwest Pacific marginal basins
linked to: New Hebrides back-arc basin