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
This entity first appeared as the object of triple T10408056 — 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 orogeny Context triple: [Inner Banda Arc, orogeny, Banda orogeny]
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A.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
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B.
Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
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C.
Pinwarian orogeny
The Pinwarian orogeny was a Precambrian mountain-building event recorded in the Canadian Shield that predates and helped set the tectonic framework for the later Grenville orogeny.
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D.
Kuunga orogeny
The Kuunga orogeny was a late Neoproterozoic to early Paleozoic mountain-building event associated with the final assembly of the Gondwana supercontinent, particularly involving collisions along the margins of East and West Gondwana.
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E.
Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Banda orogeny Target entity description: 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.
-
A.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
-
B.
Grenville orogeny
The Grenville orogeny was a major Precambrian mountain-building event that helped assemble the supercontinent Rodinia and formed the ancient core of parts of North America and other continents.
-
C.
Pinwarian orogeny
The Pinwarian orogeny was a Precambrian mountain-building event recorded in the Canadian Shield that predates and helped set the tectonic framework for the later Grenville orogeny.
-
D.
Kuunga orogeny
The Kuunga orogeny was a late Neoproterozoic to early Paleozoic mountain-building event associated with the final assembly of the Gondwana supercontinent, particularly involving collisions along the margins of East and West Gondwana.
-
E.
Variscan orogeny
The Variscan orogeny was a major late Paleozoic mountain-building event in Europe, broadly contemporaneous with the Appalachian orogeny, that resulted from the collision of continental plates during the assembly of the supercontinent Pangaea.
- F. None of above. chosen
Statements (46)
| Predicate | Object |
|---|---|
| instanceOf |
geological process
ⓘ
mountain-building event ⓘ orogeny ⓘ |
| affects |
Banda Sea crust
ⓘ
Seram region NERFINISHED ⓘ Tanimbar Islands NERFINISHED ⓘ Timor region NERFINISHED ⓘ |
| associatedWith |
Banda Arc
NERFINISHED
ⓘ
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 NERFINISHED ⓘ |
| hasConsequence |
hazardous earthquakes in eastern Indonesia
ⓘ
tsunami-generating seismic events in Banda Sea ⓘ |
| involves |
Australian Plate
NERFINISHED
ⓘ
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 NERFINISHED ⓘ |
| ongoing | true ⓘ |
| partOf | Alpine-Himalayan orogenic belt NERFINISHED ⓘ |
| 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
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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 orogeny Description of subject: 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.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.