Banda orogeny

E861924

The Banda orogeny is a mountain-building event responsible for the complex tectonic deformation and uplift associated with the collision of the Australian Plate with the Banda Arc region in eastern Indonesia.

All labels observed (1)

Label Occurrences
Banda orogeny canonical 1

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf geological process ⓘ
mountain-building event ⓘ
orogeny ⓘ
affects Banda Sea crust ⓘ
Seram region ⓘ
linked to: Seram

Tanimbar Islands ⓘ
Timor region ⓘ
linked to: Timor
associatedWith Banda Arc ⓘ
Banda Sea region ⓘ
causes crustal shortening ⓘ
exhumation of high-pressure metamorphic rocks ⓘ
folding of sedimentary sequences ⓘ
structural complexity in Banda Arc region ⓘ
thrust faulting ⓘ
uplift of orogenic belts ⓘ
characterizedBy active volcanism in Banda Arc ⓘ
high seismicity ⓘ
steeply dipping subduction zones ⓘ
tight oroclinal bending ⓘ
controls distribution of sedimentary basins in eastern Indonesia ⓘ
regional topography of Banda Arc region ⓘ
drivenBy collision of Australian Plate with Banda Arc ⓘ
geologicalAge Cenozoic ⓘ
geologicalAgeDetail Neogene ⓘ
hasConsequence hazardous earthquakes in eastern Indonesia ⓘ
tsunami-generating seismic events in Banda Sea ⓘ
involves Australian Plate ⓘ
Eurasian-affiliated microplates ⓘ
oceanic and continental lithosphere interaction ⓘ
linkedTo deformation of Australian continental margin sediments ⓘ
formation of accretionary complexes ⓘ
uplift of outer Banda Arc islands ⓘ
locatedIn eastern Indonesia ⓘ
ongoing true ⓘ
partOf Alpine-Himalayan orogenic belt ⓘ
produces mountain belts of Timor and adjacent islands ⓘ
relatedTo arc curvature of Banda Arc ⓘ
rollback of subducting slab ⓘ
subduction of Australian Plate beneath Banda Arc ⓘ
resultsIn complex tectonic deformation in eastern Indonesia ⓘ
development of forearc and backarc basins ⓘ
formation of Banda Arc orogenic system ⓘ
studiedIn plate tectonics ⓘ
structural geology ⓘ
tectonics ⓘ
tectonicSetting arc-continent collision ⓘ

How these facts were elicited

Referenced by (1)

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

Inner Banda Arc → orogeny → Banda orogeny ⓘ