Southeastern Indonesia is located at a convergent triple junction of 3 terjemahan - Southeastern Indonesia is located at a convergent triple junction of 3 Bahasa Indonesia Bagaimana mengatakan

Southeastern Indonesia is located a

Southeastern Indonesia is located at a convergent triple junction of 3 plates : the Pacific (including the Caroline
and Philippines plates), the Australian and the Southeast Asian plates (fig. 1). The age of the different basins : the
North Banda Sea (Sula Basin), the South Banda Sea (Wetar and Damar Basins) and the Weber Trough has been debated
for a long time. Their great depth was a reason to interpret them as remnants of oceanic domains either of Indian or Pacific
ocean affinities. It has now been demonstrated from geochronological studies that these basins have formed during
the Neogene [Réhault et al., 1994 ; Honthaas et al., 1998]. The crust has been sampled only in the Sula Basin, where basalts
or trachyandesites with back-arc geochemical signatures have been dredged. Their ages range from 11.4 ± 1.15 to
7.33 ± 0.18 Ma [Réhault et al., 1994 ; Honthaas et al., 1998]. The study of the magnetic anomaly pattern of these basins
confirms this interpretation and defines an age between 12.5 and 7.15 Ma for the North Banda Basin and between 6.5 to
3.5 Ma for the South Banda Basin [Hinschberger et al., 2000 ; Hinschberger et al., 2001]. Furthermore, the existence of
volcanic arcs linked to subducted slabs suggests that these basins resulted from back-arc spreading and subduction slab
roll-back. Lastly, the Weber Trough which exceeds 7 300 m in depth and is one of the deepest non subduction basins in
the world, remains enigmatic.
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Hasil (Bahasa Indonesia) 1: [Salinan]
Disalin!
Southeastern Indonesia is located at a convergent triple junction of 3 plates : the Pacific (including the Carolineand Philippines plates), the Australian and the Southeast Asian plates (fig. 1). The age of the different basins : theNorth Banda Sea (Sula Basin), the South Banda Sea (Wetar and Damar Basins) and the Weber Trough has been debatedfor a long time. Their great depth was a reason to interpret them as remnants of oceanic domains either of Indian or Pacificocean affinities. It has now been demonstrated from geochronological studies that these basins have formed duringthe Neogene [Réhault et al., 1994 ; Honthaas et al., 1998]. The crust has been sampled only in the Sula Basin, where basaltsor trachyandesites with back-arc geochemical signatures have been dredged. Their ages range from 11.4 ± 1.15 to7.33 ± 0.18 Ma [Réhault et al., 1994 ; Honthaas et al., 1998]. The study of the magnetic anomaly pattern of these basinsconfirms this interpretation and defines an age between 12.5 and 7.15 Ma for the North Banda Basin and between 6.5 to3.5 Ma for the South Banda Basin [Hinschberger et al., 2000 ; Hinschberger et al., 2001]. Furthermore, the existence ofvolcanic arcs linked to subducted slabs suggests that these basins resulted from back-arc spreading and subduction slabroll-back. Lastly, the Weber Trough which exceeds 7 300 m in depth and is one of the deepest non subduction basins inthe world, remains enigmatic.
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Hasil (Bahasa Indonesia) 2:[Salinan]
Disalin!
Southeastern Indonesia terletak di persimpangan tiga konvergen dari 3 piring: Pasifik (termasuk Caroline
piring dan Filipina), Australia, dan lempeng Asia Tenggara (gambar 1).. Usia cekungan yang berbeda:
Utara Laut Banda (Sula Basin), Banda Laut Selatan (Wetar dan Damar cekungan) dan Weber Trough telah diperdebatkan
untuk waktu yang lama. Mendalam mereka adalah alasan untuk menafsirkannya sebagai sisa-sisa dari domain kelautan baik dari India atau Pacific
afinitas laut. Sekarang telah dibuktikan dari penelitian geochronological yang cekungan telah terbentuk selama
satu Neogen [Réhault et al., 1994; Honthaas et al., 1998]. Kerak telah sampel hanya di Sula Basin, di mana basal
atau trachyandesites dengan tanda tangan geokimia-back arc telah dikeruk. Usia mereka berkisar dari 11,4 ± 1,15 untuk
7.33 ± 0.18 Ma [Réhault et al., 1994; Honthaas et al., 1998]. Studi tentang pola anomali magnetik dari cekungan ini
menegaskan penafsiran ini dan mendefinisikan usia antara 12,5 dan 7,15 Ma untuk Banda Basin Utara dan antara 6,5 sampai
3,5 Ma untuk Banda Basin Selatan [Hinschberger et al., 2000; Hinschberger et al., 2001]. Selanjutnya, keberadaan
busur vulkanik terkait dengan lempengan subduksi menunjukkan bahwa cekungan ini dihasilkan dari back-arc menyebar dan subduksi lempengan
roll-back. Terakhir, Weber Trough yang melebihi 7 300 m kedalaman dan merupakan salah satu yang paling dalam cekungan non subduksi di
dunia, tetap misterius.
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