A new sketch of the central North Banda Sea, Eastern Indonesia

Rehault, J.-P.; Malod, J.; Larue, M.; Burhanuddinn, S.; Sarmili, Lili

doi:10.1016/0743-9547(91)90078-c

Cited by 19 publications

(6 citation statements)

References 9 publications

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“…In fact, compression caused by northward convergence of the Australian plate should exist unless the Australian plate is actually two or more plates in relative motion (Cardwell and Isacks, 1978;Bowin et al, 1980). Other fragments within the Banda Basins of Eastern Indonesia have lithologic similarities to the continental Bird's Head and Australia and are thought to be trapped lithospheric "micro-continents" (Rehault et al, 1991). These fragments were supposedly strike-slip faulted into position during the middle to late Miocene.…”

Section: Geomorphology Of the Central Pacific Megatrendmentioning

confidence: 98%

“…This assumption is based mainly on low heat flow, depth of basement, and interpretation of magnetic lineations (Bowin et al, 1980;Lee and McCabe, 1986). These fragments have been considered to be of Pacific origin and also of Indian Ocean affinities (Rehault et al, 1991).…”

Section: Geomorphology Of the Central Pacific Megatrendmentioning

confidence: 99%

“…Banda Sea locator map and structural diagram (Achdan and Turkandi, 1982;Audley-Charles. 1981;Cardwell and Isaacs, 1978;Charlton et al, 1991;Delegation of Indonesia, 1994;Hall and Blundell, 1996;Hutchinson, 1989;Meyerhoff et al, 1992Meyerhoff et al, , 1996Packham, 1996;Rehault et al, 1991;Simanjuntak and Barber, 1996). The Weber…”

Section: Introductionmentioning

confidence: 95%

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The Central Pacific Megatrend

Smoot¹,

Leybourne

2001

International Geology Review

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Section: Geomorphology Of the Central Pacific Megatrendmentioning

confidence: 98%

Section: Geomorphology Of the Central Pacific Megatrendmentioning

confidence: 99%

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The Central Pacific Megatrend

Smoot¹,

Leybourne

2001

International Geology Review

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“…There are some potential active faults distributions around Indonesia Islands. The active fault features and parameters used in study based on published reports proposed by several researchers [3, [8][9][10][11][12][13][14][15][16][17][18][19][20]. General condition of the mayor tectonic features was shown in Figure 3.…”

Section: Mayor Tectonic Of Indonesia Regionmentioning

confidence: 99%

Development of Spectral Hazard Map for Indonesia with a Return Period of 2500 Years using Probabilistic Method

Asrurifak¹,

Irsyam²,

Budiono³

et al. 2010

ced

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This study is performed to develop spectral hazard map for Indonesia with a Return Period of 2500 years earthquake. It will be proposed for revision of the Indonesian hazard map in SNI-03-1726-2002 as response to the meeting organized by the Department of Public Works on 27-October-2008 in Jakarta. The meeting has decided to revise the Indonesia hazard map by referring to IBC-2006 where spectral acceleration values at Peak Ground Acceleration/PGA, 0.2 and 1.0 second with a return period of 2500 year will be applied for general buildings. The spectral hazard map was analyzed using total probability method and three dimensional (3-D) source models with recent seismotectonic parameters. Four source models were used in this analysis, namely: shallow background, deep background, fault, and subduction source models. Generally, the results of analysis show the values of PGA with a return period of 2500 years relatively higher 1.2-3.0 times than in SNI-03-1726-2002.

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“…The Banda Arc collision has been intensively studied (Bowin et al, 1980;Richardson , 1993 ), but interpretation has been hindered by uncertainties as to the origin of the Banda Sea, where water depths in excess of 5 km testify to the presence of oceanic crust in the North and South Banda basins but where high-standing ridges include continental material (Silver et al, 1985). It has been suggested that the sea is underlain by trapped Mesozoic crust (McCabe et al, 1993) but the magnetic anomaly matching on which this hypothesis is based is suspect because ofthe irregular shape ofthe oceanic area, and has not been supported dredging, which has recovered only Middle Miocene or younger rocks (Rehault et al , 1994). Since there is compelling evidence for Middle Miocene collision in the Sulawesi region, at the western margin of the sea (Bergman et al , 1996), a Banda Sea origin as a post-collisional collapse basin, on the Mediterranean model, seems more probable.…”

Section: Introductionmentioning

confidence: 99%

The Banda Sea: continental collision at the eastern end of Tethys

Milsom¹

1999

BGSM

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Continental collision in the Himalayan and Mediterranean segments of the Tethyan domain has produced regions of dramatic local extension within overall compressional environments. In the Mediterranean, deep basins have been created which are partly enclosed by orogenic belts forming arcs with total curvatures approaching 180°. These basins are floored either by attenuated continental crust (Alboran and Aegean seas) or by oceanic crust (parts of the Tyrrhenian Sea), The eastern Indonesia (Banda Arc) segment of the Tethyan collision zone has not usually been considered in terms of continent-continent collision because attention has been focussed on the presentday impact of Australia. Ther e is, however, much evidence for earlier collisions of fragments of the Australasian continent with this margin of Eurasia, and there are striking resemblances to the Mediterranean region. High standing ridges in the centre ofthe Banda Sea include continental material but water depths in excess of 5 km testify to the presence of oceanic crust in the North and South Banda basins. The 180° loop of the Banda Arc can be considered an end member in the spectrum of Tethyan collisional orogens, at the limit a t which oceanic influences (in the form of th e uncollided Indian Ocean west of Australia) remain important.

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A new sketch of the central North Banda Sea, Eastern Indonesia

Cited by 19 publications

References 9 publications

The Central Pacific Megatrend

The Central Pacific Megatrend

Development of Spectral Hazard Map for Indonesia with a Return Period of 2500 Years using Probabilistic Method

The Banda Sea: continental collision at the eastern end of Tethys

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