Banda Arc–Australian collision zone
E745514
The Banda Arc–Australian collision zone is a complex tectonic region in eastern Indonesia where the Banda volcanic arc is colliding with and overriding the northern margin of the Australian continental plate, producing intense deformation, seismicity, and mountain building.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Banda Arc–Australian collision zone canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T8616139 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Banda Arc–Australian collision zone Context triple: [Seram Trough, geologicalProvince, Banda Arc–Australian collision zone]
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A.
Inner Banda Arc
The Inner Banda Arc is a volcanic island arc in the Banda Sea region of eastern Indonesia, formed by subduction processes and comprising islands such as Atauro.
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B.
Romanche Fracture Zone
The Romanche Fracture Zone is a major transform fault and deep-sea fracture zone in the equatorial Atlantic Ocean that offsets the Mid-Atlantic Ridge and hosts one of the deepest points in the Atlantic basin.
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C.
Shackleton Fracture Zone
The Shackleton Fracture Zone is a major submarine tectonic feature in the Southern Ocean that forms part of the complex plate boundary system around the Scotia Plate near Antarctica.
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D.
Tonga–Kermadec Arc
The Tonga–Kermadec Arc is a major submarine volcanic island arc and trench system in the southwest Pacific Ocean, formed by the subduction of the Pacific Plate beneath the Indo-Australian Plate and known for its intense seismic and volcanic activity.
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E.
Owen Fracture Zone
The Owen Fracture Zone is a major transform fault system in the northwest Indian Ocean that marks part of the tectonic boundary between the Arabian and Indian plates.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Banda Arc–Australian collision zone Target entity description: The Banda Arc–Australian collision zone is a complex tectonic region in eastern Indonesia where the Banda volcanic arc is colliding with and overriding the northern margin of the Australian continental plate, producing intense deformation, seismicity, and mountain building.
-
A.
Inner Banda Arc
The Inner Banda Arc is a volcanic island arc in the Banda Sea region of eastern Indonesia, formed by subduction processes and comprising islands such as Atauro.
-
B.
Romanche Fracture Zone
The Romanche Fracture Zone is a major transform fault and deep-sea fracture zone in the equatorial Atlantic Ocean that offsets the Mid-Atlantic Ridge and hosts one of the deepest points in the Atlantic basin.
-
C.
Shackleton Fracture Zone
The Shackleton Fracture Zone is a major submarine tectonic feature in the Southern Ocean that forms part of the complex plate boundary system around the Scotia Plate near Antarctica.
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D.
Tonga–Kermadec Arc
The Tonga–Kermadec Arc is a major submarine volcanic island arc and trench system in the southwest Pacific Ocean, formed by the subduction of the Pacific Plate beneath the Indo-Australian Plate and known for its intense seismic and volcanic activity.
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E.
Owen Fracture Zone
The Owen Fracture Zone is a major transform fault system in the northwest Indian Ocean that marks part of the tectonic boundary between the Arabian and Indian plates.
- F. None of above. chosen
Statements (50)
| Predicate | Object |
|---|---|
| instanceOf |
collision zone
ⓘ
plate boundary zone ⓘ tectonic region ⓘ |
| adjacentTo |
Banda Sea
NERFINISHED
ⓘ
Banda Trench NERFINISHED ⓘ Timor Trough NERFINISHED ⓘ |
| associatedWith |
Banda Sea back-arc basin
NERFINISHED
ⓘ
Banda volcanic arc NERFINISHED ⓘ inner Banda Arc ⓘ outer Banda Arc NERFINISHED ⓘ |
| causes |
rapid uplift of Timor
ⓘ
topographic uplift of outer Banda Arc islands ⓘ |
| characterizedBy |
crustal shortening
ⓘ
fold-and-thrust belts ⓘ high seismicity ⓘ intense deformation ⓘ mountain building ⓘ strike-slip faulting ⓘ thrust faulting ⓘ |
| contains |
Seram Island
NERFINISHED
ⓘ
Tanimbar Islands NERFINISHED ⓘ Timor Island NERFINISHED ⓘ |
| deformationStyle |
oblique convergence
ⓘ
partitioned strike-slip and thrust motion ⓘ |
| geologicalFeature |
forearc basin remnants
ⓘ
high-pressure metamorphic rocks ⓘ imbricated thrust sheets ⓘ uplifted Australian continental margin ⓘ |
| involvesPlate |
Australian Plate
NERFINISHED
ⓘ
Eurasian Plate NERFINISHED ⓘ Seram microplate NERFINISHED ⓘ Sunda Plate NERFINISHED ⓘ Timor microplate NERFINISHED ⓘ |
| locatedIn |
Southeast Asia
ⓘ
eastern Indonesia ⓘ southern margin of the Banda Sea region ⓘ |
| maximumEarthquakeMagnitude | >7 ⓘ |
| overrides | northern margin of the Australian continental plate ⓘ |
| partOf | Banda Arc NERFINISHED ⓘ |
| plateConvergenceRate | approximately 6–8 cm/yr ⓘ |
| researchInterest |
arc–continent collision processes
ⓘ
orogenic wedge development ⓘ slab rollback and curvature of arcs ⓘ |
| seismicityType |
deep-focus earthquakes
ⓘ
intermediate-depth earthquakes ⓘ shallow earthquakes ⓘ |
| tectonicProcess |
arc–continent collision
ⓘ
continental underthrusting ⓘ obduction ⓘ subduction termination ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Banda Arc–Australian collision zone Description of subject: The Banda Arc–Australian collision zone is a complex tectonic region in eastern Indonesia where the Banda volcanic arc is colliding with and overriding the northern margin of the Australian continental plate, producing intense deformation, seismicity, and mountain building.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.