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.