Okinawa Trough

E234385

The Okinawa Trough is a back-arc basin in the East China Sea, located between the Ryukyu Islands and mainland Asia, known for its active tectonics and hydrothermal activity.

All labels observed (1)

Label Occurrences
Okinawa Trough canonical 5

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf back-arc basin
tectonic feature
associatedWith Eurasian Plate
Philippine Sea Plate subduction
Ryukyu Trench
boundedBy Ryukyu Islands
continental margin of China
extendsFrom western Japan
surface form: southwestern Japan region
extendsTo Taiwan, Province of China
surface form: Taiwan region
geologicalAge Cenozoic
hasBiologicalSignificance chemosynthetic fauna
hydrothermal vent ecosystems
hasCrustType thinned continental crust
transitional crust
hasEconomicInterest seafloor massive sulfide deposits
submarine mineral resources
hasFeature hydrothermal fields
hydrothermal vents
rift valleys
sediment-filled basin floor
volcanic ridges
hasGeologicalActivity active rifting
crustal extension
normal faulting
seismic activity
volcanism
isSiteOf active faulting
back-arc spreading
submarine volcanism
knownFor active tectonics
chemosynthetic biological communities
intense hydrothermal activity
submarine hydrothermal mineralization
locatedIn East China Sea
western Pacific Ocean
openingBegan Late Miocene
openingContinued Pliocene
Quaternary
parallelTo Ryukyu island arc
surface form: Ryukyu Island arc

Ryukyu Trench
partOf Ryukyu island arc
surface form: Ryukyu arc system
separates Ryukyu Islands
mainland Asia
studiedIn hydrothermal geochemistry
marine geology
plate tectonics
tectonicSetting back-arc extension
subduction-related

How these facts were elicited

Referenced by (5)

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

Ryukyu Arc hasPart Okinawa Trough
Ryukyu Arc adjacentTo Okinawa Trough
Okinawa Plate associatedWith Okinawa Trough
Ryukyu back-arc basin adjacentTo Okinawa Trough
Ryukyu subduction zone backArcBasin Okinawa Trough