Shikoku Basin

E125529

Shikoku Basin is a back-arc basin in the Philippine Sea, located south of Japan and formed by seafloor spreading behind the Izu–Bonin–Mariana volcanic arc.

All labels observed (1)

Label Occurrences
Shikoku Basin canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf back-arc basin
geologic basin
submarine basin
adjacentTo Izu–Ogasawara Trench
surface form: Izu–Bonin Trench

Nankai Trough
associatedWith Izu–Bonin Arc
surface form: Izu–Bonin–Mariana volcanic arc

Philippine Sea Plate
boundedBy Izu–Bonin Arc
surface form: Izu–Bonin Ridge

Kyushu–Palau Ridge system
surface form: Kyushu–Palau Ridge

Nankai Trough
West Philippine Basin
countryOffshoreFrom Japan
crustType oceanic crust
formedBy seafloor spreading
geologicalAge Cenozoic
hasFeature magnetic lineations from seafloor spreading
sediment-covered oceanic crust
hasMorphology abyssal plain
hasTectonicSignificance constrains timing of Izu–Bonin–Mariana arc development
records evolution of the Philippine Sea Plate
isExampleOf back-arc basin formed by subduction rollback
liesBetween Izu–Bonin Arc
surface form: Izu–Bonin Ridge and Kyushu–Palau Ridge
liesEastOf Kyushu–Palau Ridge system
surface form: Kyushu–Palau Ridge
liesNorthOf West Philippine Basin
liesWestOf Izu–Ogasawara Trench
surface form: Izu–Bonin Trench
locatedIn Philippine Sea
western Pacific Ocean
locatedSouthOf Honshu
Japan
Shikoku
namedAfter Shikoku
surface form: Shikoku Island
oceanRegion western Pacific Ocean
surface form: Northwest Pacific
openingBegan Oligocene
openingBeganApproxMa about 30 million years ago
openingEndedApproxMa about 15 million years ago
overriddenBy Eurasian Plate
partOf Philippine Sea Plate
surface form: Philippine Sea Plate oceanic crust
relatedProcess subduction of the Philippine Sea Plate
relatedTo Nankai megathrust
researchField marine geology
plate tectonics
seafloorSpreadingType back-arc spreading
spreadingCenterType extinct spreading ridge
spreadingStatus ceased
subductingUnder Eurasian Plate at the Nankai Trough
tectonicOrigin rollback of the Izu–Bonin–Mariana subduction zone
tectonicSetting back-arc region of the Izu–Bonin–Mariana arc

How these facts were elicited

Referenced by (1)

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

Philippine Sea Plate hasFeature Shikoku Basin