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.

Try in SPARQL Jump to: Surface forms Statements Referenced by

All labels observed (1)

Label Occurrences
New Hebrides back-arc basin canonical 1

Statements (30)

Predicate Object
instanceOf back-arc basin
geological feature
seafloor spreading center
associatedWith New Hebrides subduction zone NERFINISHED
Vanuatu island arc NERFINISHED
developedBehind New Hebrides volcanic arc NERFINISHED
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 NERFINISHED
isStudiedIn geophysics
marine geology
plate tectonics
isTypeOf ocean basin
locatedBehind New Hebrides island arc NERFINISHED
locatedIn Pacific Ocean
southwest Pacific Ocean NERFINISHED
partOf southwest Pacific back-arc system
relatedTo convergence between Australian Plate and Pacific Plate
subduction of the Australian Plate
tectonicSetting back-arc region

Referenced by (1)

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

New Hebrides Trench isAdjacentTo New Hebrides back-arc basin