Tanimbar Trough

E752809

The Tanimbar Trough is a deep oceanic trench and tectonic feature in the eastern Indonesian region, formed by complex subduction and collision processes between the Indo-Australian and Eurasian plates.

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All labels observed (1)

Label Occurrences
Tanimbar Trough canonical 1

Statements (39)

Predicate Object
instanceOf oceanic trench
tectonic feature
associatedWith earthquakes
seismic activity
tsunami hazard potential
bathymetricFeature deep linear depression
convergentBoundaryBetween Eurasian Plate NERFINISHED
Indo-Australian Plate NERFINISHED
country Indonesia
formedBy collision processes
subduction
geodynamicContext arc-continent collision in Banda Arc
geologicalAge Cenozoic
geologicalProcess crustal deformation
plate convergence
sediment accretion
knownFor complex subduction geometry
transition from subduction to collision
locatedIn Banda Sea NERFINISHED
Southeast Asia
eastern Indonesian region
marginType active continental margin
maximumDepth over 6000 m
near Tanimbar Islands NERFINISHED
ocean Indian Ocean–Pacific transition zone NERFINISHED
partOf Banda Arc region NERFINISHED
Indo-Australian–Eurasian plate boundary zone NERFINISHED
relatedFeature Banda Trench NERFINISHED
Seram Trough NERFINISHED
Timor Trough NERFINISHED
researchField marine geology
plate tectonics
seismology
sedimentaryEnvironment trench fill sediments
separates Australian continental margin
Banda forearc region NERFINISHED
tectonicRole accommodates convergence between Australia and Southeast Asia
tectonicSetting convergent plate margin
subduction–collision zone

Referenced by (1)

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

Seram Trough relatedStructure Tanimbar Trough