back-arc Lau Basin

E237726

The back-arc Lau Basin is an actively spreading oceanic basin in the southwest Pacific formed behind the Tonga-Kermadec subduction zone, notable for its intense volcanism and hydrothermal activity.

All labels observed (1)

Label Occurrences
back-arc Lau Basin canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf back-arc basin
oceanic basin
adjacentTo Kermadec Trench
Tonga Trench
associatedWith Australian Plate
Pacific Plate
Tonga Plate
boundedBy Tonga–Kermadec Arc
surface form: Kermadec Ridge

Lau Ridge
Tonga Ridge
formedBehind Tonga-Kermadec subduction system
surface form: Tonga-Kermadec subduction zone
formedBy rollback of the Tonga-Kermadec subduction zone
geologicalAge Cenozoic
hasActivity hydrothermal activity
intense volcanism
hasBiologicalFeature chemosynthetic vent communities
hasCrustType back-arc oceanic crust
hasFeature back-arc volcanoes
hydrothermal vent fields
spreading centers
volcanic ridges
hasGeologicalProcess back-arc spreading
subduction-related magmatism
hasHydrothermalSystem high-temperature hydrothermal vents
sulfide-rich vent deposits
hasMagmaSource depleted upper mantle
subduction-modified mantle wedge
hasMorphology complex network of spreading centers and transform faults
hasSeafloorType young oceanic crust
hasTectonicActivity active seafloor spreading
hasVolcanismType arc-like volcanism
subduction-influenced MORB-like volcanism
influences geochemical cycles of sulfur and metals in the southwest Pacific
isExampleOf active back-arc spreading system
subduction-related hydrothermal province
isPartOf Tonga-Kermadec subduction system
surface form: Tonga-Lau back-arc system
locatedIn Pacific Ocean
southwest Pacific Ocean
monitoredBy marine geophysical surveys
oceanographic expeditions
researchInterest extremophile vent ecosystems
hydrothermal mineralization
subduction and back-arc spreading processes
spreadingRate one of the fastest back-arc spreading rates on Earth
spreadingStyle asymmetric back-arc spreading
tectonicSetting back-arc region of Tonga-Kermadec subduction system
waterDepth deep-sea basin

How these facts were elicited

Referenced by (1)

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