Mariana Trough

E288645

The Mariana Trough is a back-arc basin in the western Pacific Ocean formed by seafloor spreading behind the Mariana subduction zone.

All labels observed (1)

Label Occurrences
Mariana Trough canonical 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf back-arc basin
geological feature
oceanic basin
associatedWith Izu–Bonin–Mariana Trench system
surface form: Izu–Bonin–Mariana subduction system

Mariana Island Arc
surface form: Mariana Arc
behind Mariana Trench
Mariana subduction zone
boundaryOf Pacific Plate
Philippine Sea Plate
floorType oceanic crust
formedBy seafloor spreading
geologicalProcess extension of overriding plate
hasFeature hydrothermal vent fields
rifted arc crust
spreading ridge
transform faults
volcanic seamounts
linkedTo subduction of the Pacific Plate beneath the Philippine Sea Plate
locatedIn Philippine Sea
western Pacific Ocean
magmatism basaltic volcanism
ocean Pacific Ocean
orientation roughly north–south
parallelTo Mariana Island Arc
surface form: Mariana island arc
partOf western Pacific back-arc basins
researchInterest back-arc spreading dynamics
subduction-related magmatism
spreadingType slow to intermediate spreading
tectonicRegime extensional
tectonicSetting back-arc spreading center

How these facts were elicited

Referenced by (1)

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

Mariana subduction zone associatedWith Mariana Trough