Eurasian Plate at the Nankai Trough

E542011

The Eurasian Plate at the Nankai Trough is a major tectonic plate margin off southwestern Japan where intense subduction-driven seismic and volcanic activity occurs.

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Statements (46)

Predicate Object
instanceOf plate margin
subduction zone
tectonic plate boundary
adjacentTo Philippine Sea Plate NERFINISHED
associatedWith Japanese island arc system
Nankai Trough NERFINISHED
Nankai accretionary prism
Southwest Japan forearc
causes large interplate earthquakes
tsunamis affecting southwestern Japan
drivenBy subduction of the Philippine Sea Plate beneath the Eurasian Plate
formsBoundaryType oceanic-continental convergent margin
hasActivity intense seismic activity
megathrust earthquakes
tsunamigenic earthquakes
volcanic activity
hasHazard great earthquake potential
strong ground shaking in southwest Japan
tsunami hazard
hasProcess accretionary prism formation
megathrust faulting
seismic coupling
subduction
locatedIn southwestern Japan
locatedOffCoastOf Honshu NERFINISHED
Kyushu NERFINISHED
Shikoku NERFINISHED
monitoredBy Japanese seismic networks
ocean-bottom seismometers
near Kii Peninsula NERFINISHED
Shikoku Basin NERFINISHED
overrides Philippine Sea Plate NERFINISHED
partOf Eurasian Plate NERFINISHED
relatedEvent 1854 Ansei-Nankai earthquake NERFINISHED
1854 Ansei-Tokai earthquake NERFINISHED
1944 Tonankai earthquake NERFINISHED
1946 Nankai earthquake NERFINISHED
Nankai megathrust earthquakes NERFINISHED
relevantTo Japanese disaster mitigation planning
plate tectonics research
subduction zone seismology
studiedBy Integrated Ocean Drilling Program NERFINISHED
International Ocean Discovery Program NERFINISHED
Japan Agency for Marine-Earth Science and Technology NERFINISHED
subductsWithRespectTo Philippine Sea Plate NERFINISHED
tectonicSetting convergent plate boundary

Referenced by (1)

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

Shikoku Basin subductingUnder Eurasian Plate at the Nankai Trough