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.

All labels observed (1)

Label Occurrences
Tanimbar Trough canonical 1

How this entity was disambiguated

Statements (39)

Predicate Object
instanceOf oceanic trench ⓘ
tectonic feature ⓘ
associatedWith earthquakes ⓘ
seismic activity ⓘ
tsunami hazard potential ⓘ
bathymetricFeature deep linear depression ⓘ
convergentBoundaryBetween Eurasian Plate ⓘ
Indo-Australian Plate ⓘ
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 ⓘ
Southeast Asia ⓘ
eastern Indonesian region ⓘ
marginType active continental margin ⓘ
maximumDepth over 6000 m ⓘ
near Tanimbar Islands ⓘ
ocean Indian Ocean–Pacific transition zone ⓘ
partOf Banda Arc region ⓘ
linked to: Banda region

Indo-Australian–Eurasian plate boundary zone ⓘ
relatedFeature Banda Trench ⓘ
Seram Trough ⓘ
Timor Trough ⓘ
researchField marine geology ⓘ
plate tectonics ⓘ
seismology ⓘ
sedimentaryEnvironment trench fill sediments ⓘ
separates Australian continental margin ⓘ
Banda forearc region ⓘ
tectonicRole accommodates convergence between Australia and Southeast Asia ⓘ
tectonicSetting convergent plate margin ⓘ
subduction–collision zone ⓘ

How these facts were elicited

Referenced by (1)

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

Seram Trough → relatedStructure → Tanimbar Trough ⓘ