Tasman Basin

E90974

The Tasman Basin is a deep oceanic basin on the seafloor between Australia and New Zealand, forming a major structural and sedimentary feature of the Tasman Sea.

All labels observed (2)

Label Occurrences
East Australian continental margin 1
Tasman Basin canonical 1

How this entity was disambiguated

Statements (44)

Predicate Object
instanceOf geologic basin
oceanic basin
submarine basin
adjacentTo Lord Howe Rise Basin system
linked to: Lord Howe Rise

New Caledonia Basin (to the north via regional system)
age Mesozoic-Cenozoic
basementType oceanic crust
boundedBy East Australian continental margin
linked to: Tasman Basin

Lord Howe Rise
New Zealand continental margin
linked to: Campbell Plateau

Norfolk Ridge
climateInfluence Southern Ocean circulation (indirect)
continentNearby Australia
Zealandia
linked to: Terra Australis
countryOffshoreFrom Australia
New Zealand
floorType abyssal plain
formedBy rifting between Australia and Zealandia
seafloor spreading
geologicSetting passive continental margin
hasFeature sediment drifts
submarine channels
hydrographicContext South Pacific gyre system
locatedBetween Australia
New Zealand
locatedIn Tasman Sea
mainFormationPeriod Late Cretaceous
maximumWaterDepth over 5000 m
namedAfter Tasman Sea
partOf Southwest Pacific Ocean
seafloor of the Tasman Sea
relatedTo opening of the Tasman Sea
researchField marine geology
plate tectonics
sedimentaryFill pelagic sediments
thick marine sediments
turbidites
separates Zealandia microcontinent
eastern Australia
studiedBy multibeam bathymetric mapping
seismic reflection surveys
tectonicPlate Indo-Australian Plate
Pacific Plate (eastern margin vicinity)
linked to: Pacific Plate
underlies central Tasman Sea

How these facts were elicited

Referenced by (2)

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

Tasman Sea contains Tasman Basin
Tasman Basin boundedBy East Australian continental margin
linked to: Tasman Basin