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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.

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  • Bandabogen (de)
  • Banda Arc (en)
  • Busur Banda (in)
  • Arco vulcânico de Banda (pt)
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  • 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)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Banda-arc-cross-section.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Banda_Arc_tectonic_map.jpg
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