Banda Arc (original) (raw)
Der Bandabogen besteht aus zwei Inselketten im Westen des Malaiischen Archipels, die durch die Kollision der Australischen mit der Eurasischen Platte entstanden sind.
| Property | Value |
|---|---|
| dbo:abstract | Der Bandabogen besteht aus zwei Inselketten im Westen des Malaiischen Archipels, die durch die Kollision der Australischen mit der Eurasischen Platte entstanden sind. (de) The Banda Arc (main arc, Inner, and Outer) is a set of island arcs in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active arc is located on what appears to be oceanic crust whereas the associated subduction trench is underlain by continental crust. The convergence of the Indo-Australian plates and Eurasia resulted in the formation of the Sunda and Banda island arcs. The transitional zone between the arcs is located south of Flores Island and is characterized by the change in the tectonic regime along the boundary. (en) Busur Banda adalah busur vulkanik yang aktif dan sangat kompleks. Disebut sangat kompleks karena busur Banda memiliki arah subduksi melengkung sebesar 180 derajat. Meskipun studi geologi dan geofisika telah banyak dilakukan, banyak aspek geologi busur Banda tetap belum diketahui dengan baik, dan bahkan masih merupakan subyek kontraversi para ahli. Hal yang paling dikontraversikan adalah busur Banda, yaitu apakah busur tersebut merupakan subduksi antara 2 lempeng kerak bumi (Hamilton, Katili), atau merupakan triple junction antara 3 buah lempeng melalui subduksi-sesar transform (Cardwell dan Isacs). Busur Banda dicirikan oleh 2 ridge melingkar (setengah lingkaran) yang konsentris. Busur Banda adalah formasi geologi di dasar laut banda yang berbentuk busur sepanjang 1000 km dan melengkung 180 derajat. Bentuknya seperti ia ditabrak sesuatu dari barat dengan sangat kuat sehingga melengkung demikian. Deformasi menyebabkan elevasi yang cepat pada kepulauan di busur Banda, terutama yang terbesar yaitu pulau Seram dan Timor, dimana keduanya muncul dari beberapa kilometer di bawah permukaan laut hingga sekarang. Hanya dalam beberapa juta tahun, kedua pulau ini sudah terangkat 3 km di atas permukaan laut. (in) O arco vulcânico de Banda, na Indonésia, é o cordão de ilhas que se estende desde a ilha de Java até à ilha de Buru (nas Molucas), englobando o Mar de Banda, é a região onde as placas tectónicas da Austrália e do Pacífico se encontram com a Placa Euroasiática. As ilhas internas do arco são vulcânicas e, neste caso, as do sul (também chamadas as pequenas ilhas de Sonda - Flores, Solor, Lomblen, Pantar e Alor) formam com as exteriores, não-vulcânicas (Sumba, Roti, Sawu e Timor), o Mar de Savu. (pt) |
| dbo:thumbnail | wiki-commons:Special:FilePath/Banda_Arc_tectonic_map.jpg?width=300 |
| dbo:wikiPageID | 37683378 (xsd:integer) |
| dbo:wikiPageLength | 5976 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID | 1033318595 (xsd:integer) |
| dbo:wikiPageWikiLink | dbc:Outer_Banda_Arc dbr:Indo-Australian_Plate dbr:Island_arcs dbr:Continent dbr:Greater_Sunda_Islands dbr:Continental_crust dbr:Continental_margin dbr:Damar_Island dbr:Solor_Archipelago dbr:Plate_tectonic dbr:Lesser_Sunda_Islands dbr:Leti_Islands dbr:Aru_Islands dbr:Volcanic_arc dbr:Plate_tectonics dbr:Sunda_Arc dbr:Sunda_Islands dbr:Sunda_Trench dbr:Sundaland dbr:Timor dbr:Wetar dbr:Ambon_Island dbr:Earth dbr:Alor_Archipelago dbc:Archipelagoes_of_Indonesia dbc:Inner_Banda_Arc dbr:Eurasia dbr:Eurasian_plate dbr:Flores dbr:Banda_Sea_Plate dbr:Barat_Daya_Islands dbc:Arcs_of_Indonesia dbc:Island_arcs dbr:Pacific_Plate dbr:Fold_(geology) dbr:Island_arc dbr:Island dbr:Babar_Islands dbr:Tectonics dbr:Craton dbr:Subduction dbc:Plate_tectonics dbr:Kai_Islands dbr:Indonesia dbr:Oceanic_trench dbr:Seram_Island dbr:Mantle_(geology) dbr:Rote_Island dbr:Volcano dbr:Indo-Australian_plate dbr:Tanimbar_Islands dbr:Oceanic_crust dbr:Structural_geology dbr:Islands_of_Indonesia dbr:Komodo_Island dbr:Savu_Island dbr:Buru_Island dbr:File:Banda-arc-cross-section.jpg dbr:File:Banda_Arc_tectonic_map.jpg dbr:Kekeh-besar |
| dbp:wikiPageUsesTemplate | dbt:Authority_control dbt:Cite_journal dbt:Convert dbt:Coord dbt:Reflist dbt:Short_description dbt:Wikibooks |
| dcterms:subject | dbc:Outer_Banda_Arc dbc:Archipelagoes_of_Indonesia dbc:Inner_Banda_Arc dbc:Arcs_of_Indonesia dbc:Island_arcs dbc:Plate_tectonics |
| gold:hypernym | dbr:Set |
| georss:point | -8.9827 125.321 |
| rdf:type | owl:Thing yago:WikicatArchipelagoesOfIndonesia yago:WikicatArchipelagoesOfTheIndianOcean yago:WikicatLesserSundaIslands geo:SpatialThing yago:Archipelago109203827 yago:Island109316454 yago:Land109334396 yago:Object100002684 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity |
| rdfs:comment | Der Bandabogen besteht aus zwei Inselketten im Westen des Malaiischen Archipels, die durch die Kollision der Australischen mit der Eurasischen Platte entstanden sind. (de) The Banda Arc (main arc, Inner, and Outer) is a set of island arcs in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active arc is located on what appears to be oceanic crust whereas the associated subduction trench is underlain by continental crust. The convergence of the Indo-Australian plates and Eurasia resulted in the formation of the Sunda and Banda island arcs. The transitional zone between the arcs is located south of Flores Island and is characterized by the change in the tectonic regime along the boundary. (en) O arco vulcânico de Banda, na Indonésia, é o cordão de ilhas que se estende desde a ilha de Java até à ilha de Buru (nas Molucas), englobando o Mar de Banda, é a região onde as placas tectónicas da Austrália e do Pacífico se encontram com a Placa Euroasiática. As ilhas internas do arco são vulcânicas e, neste caso, as do sul (também chamadas as pequenas ilhas de Sonda - Flores, Solor, Lomblen, Pantar e Alor) formam com as exteriores, não-vulcânicas (Sumba, Roti, Sawu e Timor), o Mar de Savu. (pt) Busur Banda adalah busur vulkanik yang aktif dan sangat kompleks. Disebut sangat kompleks karena busur Banda memiliki arah subduksi melengkung sebesar 180 derajat. Meskipun studi geologi dan geofisika telah banyak dilakukan, banyak aspek geologi busur Banda tetap belum diketahui dengan baik, dan bahkan masih merupakan subyek kontraversi para ahli. Hal yang paling dikontraversikan adalah busur Banda, yaitu apakah busur tersebut merupakan subduksi antara 2 lempeng kerak bumi (Hamilton, Katili), atau merupakan triple junction antara 3 buah lempeng melalui subduksi-sesar transform (Cardwell dan Isacs). Busur Banda dicirikan oleh 2 ridge melingkar (setengah lingkaran) yang konsentris. Busur Banda adalah formasi geologi di dasar laut banda yang berbentuk busur sepanjang 1000 km dan melengkung 18 (in) |
| rdfs:label | Bandabogen (de) Banda Arc (en) Busur Banda (in) Arco vulcânico de Banda (pt) |
| owl:sameAs | freebase:Banda Arc yago-res:Banda Arc wikidata:Banda Arc dbpedia-de:Banda Arc dbpedia-id:Banda Arc dbpedia-pt:Banda Arc https://global.dbpedia.org/id/4VaGX |
| geo:geometry | POINT(125.32099914551 -8.9827003479004) |
| geo:lat | -8.982700 (xsd:float) |
| geo:long | 125.320999 (xsd:float) |
| prov:wasDerivedFrom | wikipedia-en:Banda_Arc?oldid=1033318595&ns=0 |
| foaf:depiction | wiki-commons:Special:FilePath/Banda-arc-cross-section.jpg wiki-commons:Special:FilePath/Banda_Arc_tectonic_map.jpg |
| foaf:isPrimaryTopicOf | wikipedia-en:Banda_Arc |
| is dbo:wikiPageDisambiguates of | dbr:Arc |
| is dbo:wikiPageRedirects of | dbr:Inner_Banda_Arc dbr:Outer_Banda_Arc |
| is dbo:wikiPageWikiLink of | dbr:Caraulun_River dbr:List_of_archipelagos dbr:July_2018_Lombok_earthquake dbr:1852_Banda_Sea_earthquake dbr:Emperor_of_China_(volcano) dbr:Geography_of_Indonesia dbr:Greater_Sunda_Islands dbr:Mount_Sinabung dbr:Mount_Wurlali dbr:Lesser_Sunda_Islands dbr:Collision_zone dbr:Sunda_Arc dbr:Sunda_Islands dbr:Sunda_Trench dbr:Sundaland dbr:2004_Alor_earthquake dbr:Banda_Sea_Islands_moist_deciduous_forests dbr:5_August_2018_Lombok_earthquake dbr:British_Institutions_Reflection_Profiling_Syndicate dbr:North_Laclo_River dbr:Flores_Back_Arc_Thrust_Fault dbr:Ashy_flowerpecker dbr:Manuk dbr:Arc dbr:Kisar dbr:List_of_volcanoes_by_elevation dbr:Ultra-high-pressure_metamorphism dbr:Inner_Banda_Arc dbr:Outer_Banda_Arc |
| is foaf:primaryTopic of | wikipedia-en:Banda_Arc |
