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Crustal Structure Along Sunda-Banda Arc Transition Zone from Teleseismic Receiver Functions

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
We analyzed receiver function of teleseismic events recorded at twelve Indonesian-GEOFON (IA-GE) broadband stations using nonlinear Neighbourhood Algorithm (NA) inversion and H-k stacking methods to estimate crustal thickness, Vp/Vs ratios and S-wave velocity structure along Sunda-Banda arc transition zone. We observed crustal thickness of 34-37 km in Timor Island, which is consistent with the previous works. The thick crust (> 30 km) is also found beneath Sumba and Flores Islands, which might be related to the arc-continent collision causing the thickened crust. In Timor and Sumba Islands, we observed high Vp/Vs ratio (> 1.84) with low velocity zone that might be associated with the presence of mafic and ultramafic materials and fluid filled fracture zone. The high Vp/Vs ratio observed at Sumbawa and Flores volcanic Islands might be an indication of partial melt related to the upwelling of hot asthenosphere material through the subducted slab.
Czasopismo
Rocznik
Strony
2020--2050
Opis fizyczny
Bibliogr. 61 poz.
Twórcy
autor
  • Graduate Research on Earthquake and Active Tectonics (GREAT), Bandung Institute of Technology (ITB), Bandung, Indonesia
  • Research Centre for Physics – Indonesian Institute of Sciences (LIPI), Tangerang Selatan, Indonesia
  • Research Centre for Geotechnology – LIPI, Bandung, Indonesia
  • Faculty of Earth Sciences and Technology, ITB, Bandung, Indonesia
autor
  • Graduate Research on Earthquake and Active Tectonics (GREAT), Bandung Institute of Technology (ITB), Bandung, Indonesia
autor
  • Faculty of Mining and Petroleum Engineering, ITB, Bandung, Indonesia
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Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c4133806-7fab-40e9-8f8e-10af01113d14
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