Pacific–Indo-Australian region

E745513

The Pacific–Indo-Australian region is a tectonically active marine area where the Pacific and Indo-Australian plates interact, giving rise to complex subduction zones, deep-sea trenches, and frequent earthquakes and volcanism.

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Statements (48)

Predicate Object
instanceOf marine region
plate boundary zone
tectonic region
adjacentTo Indonesia NERFINISHED
New Guinea region NERFINISHED
New Hebrides Arc NERFINISHED
Philippine Sea region
Sunda Arc NERFINISHED
Tonga–Kermadec Arc NERFINISHED
geodynamicSetting interaction of Pacific and Indo-Australian plates
oceanic–continental convergence
oceanic–oceanic convergence
hasBoundaryType convergent plate boundary
subduction zone boundary
hasFeature back-arc basins
complex subduction zones
deep-sea trenches
island arcs
hasInteractingPlate Australian Plate NERFINISHED
Indian Plate NERFINISHED
Indo-Australian Plate NERFINISHED
Pacific Plate NERFINISHED
hasProcess arc magmatism
crustal deformation
seafloor seismicity
slab subduction
hasTrench Java Trench NERFINISHED
Kermadec Trench NERFINISHED
New Hebrides Trench NERFINISHED
Puysegur Trench NERFINISHED
Sunda Trench NERFINISHED
Tonga Trench NERFINISHED
influences seismic hazard in surrounding coastal countries
tsunami generation in the Indo-Pacific
locatedIn Pacific Ocean
Southeast Asia
eastern Indian Ocean NERFINISHED
southwestern Pacific
partOf Pacific Ring of Fire
seismicity frequent large earthquakes
studiedIn marine geology
plate tectonics
seismology
tectonicActivity earthquakes
plate convergence
subduction
volcanism
volcanicActivity frequent explosive eruptions

Referenced by (1)

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

Seram Trough liesInOcean Pacific–Indo-Australian region