Banda Basin

E204040

The Banda Basin is a deep oceanic basin in eastern Indonesia, known for its complex tectonic setting and very deep waters within the Banda Sea region.

All labels observed (1)

Label Occurrences
Banda Basin canonical 1

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf geological formation
oceanic basin
tectonic basin
adjacentTo Banda Arc
Seram Trough
Timor Trough
age Cenozoic
associatedWith Banda Sea Plate
collision between Australian continental margin and Banda Arc
basinType oceanic
bathymetryFeature deep central basin of Banda Sea
characteristic complex crustal structure
high seismicity region
steep bathymetry
very deep waters
country Indonesia
crustType oceanic crust
formedBy back-arc basin formation
subduction-related processes
formedDuring Neogene
geologicalProvince Banda Arc
knownFor active deformation
complex tectonic evolution
deep marine sedimentary sequences
linkedTo arc-continent collision
back-arc extension
locatedIn Banda Sea
eastern Indonesia
locatedOn Australian Plate margin
Eurasian Plate margin
maximumDepth greater than 5000 m
near Banda Islands
Seram
surface form: Seram Island

Timor
surface form: Timor Island
ocean Pacific Ocean region
eastern Indian Ocean region
partOf Banda Sea
surface form: Banda Sea region

Southeast Asia
region Maluku Islands
surface form: Maluku Islands region
researchField marine geology
plate tectonics
seismology
tectonicSetting complex
convergent margin
subduction zone
waterBody Banda Sea

How these facts were elicited

Referenced by (1)

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

Banda Sea hasFeature Banda Basin