Banda Arc

Short description: Set of island arcs in eastern Indonesia

Banda Arc tectonic map

The Banda Arc (main arc, Inner, and Outer) is a dual chain of islands in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active volcanic arc is mounted on stretched continental and oceanic crust whereas the associated subduction trench is underlain by continental crust, which has subducted deep enough to contaminate the volcanic arc with continental melts.[1] 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. in the Timor Region.[2][3]

## Contents

* 1 Terminology
* 2 Inner and outer arcs
* 3 See also
* 4 References

## Terminology

Some academic literature refers to the arcs by location – so that the main arc can be referred to as the 'southern',[4] the 'western' [5] Situated at the centre of three converging and colliding major tectonic plates, Indo-Australia, Eurasia, Pacific, the Banda arc includes young oceanic crust enclosed by a volcanic inner arc, outer arc islands and a trough parallel to the Australian continental margin. It is a complex subduction setting (where one plate moves under another, sinking into the Earth's mantle), with possibly the largest fold on Earth, extending to a depth of about 650 km (404 mi), in a subducted plate.[6]

## Inner and outer arcs

Cross section between inner and outer arc

The Banda Arc is a double island arc formed by the collision of the Indo-Australian plate with the Eurasian plate. Principal islands include Timor, Flores, and Seram.

* The Inner Banda Arc consists of a string of recent and active volcanic islands from Komodo to Kekeh-besar of the Barat Daya Islands, including Flores, Solor, Alor, Wetar, and Damar.
* The Outer Banda Arc consists of an accretionary wedge of Australian continental margin cover units that were scrapped off the Australian plate and added to the southern edge of the Asian plate. The Banda arc-continent collision is still active and converging at a rate of 7 cm/a. It stretches from Savu through Rote, Timor, Leti, Babar, Tanimbar, and the Kai Islands, before turning west to Seram, Ambon, and Buru. The outer arc is geologically associated with the Australian continent, though it is a more recent accretion than the neighbouring Aru Islands.

The resulting feature is a 180-degree island arc, which is more than 1,000 kilometres (620 miles) long. Geographically, it stretches across eastern Indonesia, and is delimited by an active inner volcanic arc. The outer arc contains numerous islands, and its internal geologic structure contains young oceanic crust exclusively.[7]

## See also

* Weber Deep
* Banda Sea Plate
* Islands of Indonesia
* Oceanic trench
* Plate tectonic
* Sunda Arc
* Sunda Islands
* Greater Sunda Islands
* Lesser Sunda Islands
* Sundaland
* Sunda Trench

## References

1. ↑ D. J. Whitford; P. A. Jezek (1979). "Origin of late-cenozoic lavas from the Banda arc, Indonesia: Trace element and Sr isotope evidence". Contributions to Mineralogy and Petrology 68 (2): 141–150. doi:10.1007/BF00371896. Bibcode: 1979CoMP...68..141W.
2. ↑ "The Nature of the Banda Arc-Continent Collision". doi:10.1007/978-3-540-88558-0_7.
3. ↑ A. Shulgin; H. Kopp; C. Mueller; E. Lueschen; L. Planert; M. Engels; E. R. Flueh; A. Krabbenhoeft et al. (May 27, 2009). "Sunda-Banda arc transition, Incipient continent-island arc collision (northwest Australia)". Geophysical Research Letters 36 (10): L10304. doi:10.1029/2009gl037533. Bibcode: 2009GeoRL..3610304S.
4. ↑ Ely, Kim Susan (2009), Geochronology of Timor-Leste and seismo-tectonics of the southern Banda Arc, http://trove.nla.gov.au/work/37054964, retrieved 21 December 2014
5. ↑ Chamalaun, F. H; Sunata, Wahyu; Institute for Australasian Geodynamics; Flinders University. School of Earth Sciences; Workshop on Palaeomagnetic Research in Southeast and East Asia (1982 : Kuala Lumpur, Malaysia) (1982), Progress report on the paleomagnetism of the Western Banda Arc system, Institute for Australasian Geodynamics, http://trove.nla.gov.au/work/8321009, retrieved 21 December 2014
6. ↑ University of Royal Holloway London (July 27, 2010). "Indonesia's puzzling Banda arc: New findings explain mystery behind geological development".
7. ↑ Tudor Vieru (6 Aug 2010). "Origins of the Banda Arc Explained". http://news.softpedia.com/news/Origins-of-the-Banda-Arc-Explained-151114.shtml.

* Audley-Charles, MG (1986). "Timor–Tanimbar Trough: the foreland basin of the evolving Banda orogen". Spec. Publs Int. Ass. Sediment 8: 91–102.

* Harris, RA (2011). "The Nature of the Banda Arc–Continent Collision in the Timor Region". Arc-Continent Collision. Frontiers in Earth Sciences. pp. 163–211. doi:10.1007/978-3-540-88558-0_7. ISBN 978-3-540-88557-3.

[ ⚑ ]  8°58′58″S 125°19′16″E﻿ / ﻿8.9827°S 125.3210°E﻿ / -8.9827; 125.3210

0.00

(0 votes)

Original source: https://en.wikipedia.org/wiki/Banda Arc. Read more

|

Retrieved from "https://handwiki.org/wiki/index.php?title=Earth:Banda_Arc&oldid=3291935"