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Title: Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis

Abstract

We analyzed receiver functions to estimate the crustal thickness and velocity structure beneath two stations of Geofon (GE) network in the Sunda-Banda arc transition zone. The stations are located in two different tectonic regimes: Sumbawa Island (station PLAI) and Timor Island (station SOEI) representing the oceanic and continental characters, respectively. We analyzed teleseismic events of 80 earthquakes to calculate the receiver functions using the time-domain iterative deconvolution technique. We employed 2D grid search (H-κ) algorithm based on the Moho interaction phases to estimate crustal thickness and Vp/Vs ratio. We also derived the S-wave velocity variation with depth beneath both stations by inverting the receiver functions. We obtained that beneath station PLAI the crustal thickness is about 27.8 km with Vp/Vs ratio 2.01. As station SOEI is covered by very thick low-velocity sediment causing unstable solution for the inversion, we modified the initial velocity model by adding the sediment thickness estimated using high frequency content of receiver functions in H-κ stacking process. We obtained the crustal thickness is about 37 km with VP/Vs ratio 2.2 beneath station SOEI. We suggest that the high Vp/Vs in station PLAI may indicate the presence of fluid ascending from the subducted plate to the volcanic arc, whereasmore » the high Vp/Vs in station SOEI could be due to the presence of sediment and rich mafic composition in the upper crust and possibly related to the serpentinization process in the lower crust. We also suggest that the difference in velocity models and crustal thicknesses between stations PLAI and SOEI are consistent with their contrasting tectonic environments.« less

Authors:
 [1];  [2]; ;  [3]; ;  [4];  [5]
  1. Graduate Research on Earthquake and Active Tectonics (GREAT), Bandung Institute of Technology, Jalan Ganesha 10, Bandung 40132 (Indonesia)
  2. (LIPI), Kompleks Puspiptek Serpong, Tangsel 15314, Banten Indonesia (Indonesia)
  3. Research Centre for Geotechnology - Indonesian Institute of Sciences (LIPI), Jl. Sangkuriang (Kompleks LIPI) Bandung 40135 (Indonesia)
  4. Faculty of Mining and Petroleum Engineering ITB, Jalan Ganesha 10, Bandung 40132 (Indonesia)
  5. Research Centre for Physics - Indonesian Institute of Sciences (LIPI), Kompleks Puspiptek Serpong, Tangsel 15314, Banten Indonesia (Indonesia)
Publication Date:
OSTI Identifier:
22391569
Resource Type:
Journal Article
Journal Name:
AIP Conference Proceedings
Additional Journal Information:
Journal Volume: 1658; Journal Issue: 1; Conference: ISEDM 2014: 4. International Sympsoium on Earthquake and Disaster Mitigation 2014, Bandung (Indonesia), 11-12 Nov 2014; Other Information: (c) 2015 AIP Publishing LLC; Country of input: International Atomic Energy Agency (IAEA); Journal ID: ISSN 0094-243X
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; 71 CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS; ALGORITHMS; DEPTH; EARTHQUAKES; GEOPHYSICS; ISLANDS; ITERATIVE METHODS; PLATES; SEDIMENTS; SEISMIC DETECTION; SEISMIC S WAVES; SEISMICITY; SEISMOLOGY; THICKNESS; VARIATIONS; ZONES

Citation Formats

Syuhada, E-mail: hadda9@gmail.com, Research Centre for Physics - Indonesian Institute of Sciences, Hananto, Nugroho D., Handayani, Lina, Puspito, Nanang T, Yudistira, Tedi, and Anggono, Titi. Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis. United States: N. p., 2015. Web. doi:10.1063/1.4915016.
Syuhada, E-mail: hadda9@gmail.com, Research Centre for Physics - Indonesian Institute of Sciences, Hananto, Nugroho D., Handayani, Lina, Puspito, Nanang T, Yudistira, Tedi, & Anggono, Titi. Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis. United States. doi:10.1063/1.4915016.
Syuhada, E-mail: hadda9@gmail.com, Research Centre for Physics - Indonesian Institute of Sciences, Hananto, Nugroho D., Handayani, Lina, Puspito, Nanang T, Yudistira, Tedi, and Anggono, Titi. Fri . "Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis". United States. doi:10.1063/1.4915016.
@article{osti_22391569,
title = {Crustal structure beneath two seismic stations in the Sunda-Banda arc transition zone derived from receiver function analysis},
author = {Syuhada, E-mail: hadda9@gmail.com and Research Centre for Physics - Indonesian Institute of Sciences and Hananto, Nugroho D. and Handayani, Lina and Puspito, Nanang T and Yudistira, Tedi and Anggono, Titi},
abstractNote = {We analyzed receiver functions to estimate the crustal thickness and velocity structure beneath two stations of Geofon (GE) network in the Sunda-Banda arc transition zone. The stations are located in two different tectonic regimes: Sumbawa Island (station PLAI) and Timor Island (station SOEI) representing the oceanic and continental characters, respectively. We analyzed teleseismic events of 80 earthquakes to calculate the receiver functions using the time-domain iterative deconvolution technique. We employed 2D grid search (H-κ) algorithm based on the Moho interaction phases to estimate crustal thickness and Vp/Vs ratio. We also derived the S-wave velocity variation with depth beneath both stations by inverting the receiver functions. We obtained that beneath station PLAI the crustal thickness is about 27.8 km with Vp/Vs ratio 2.01. As station SOEI is covered by very thick low-velocity sediment causing unstable solution for the inversion, we modified the initial velocity model by adding the sediment thickness estimated using high frequency content of receiver functions in H-κ stacking process. We obtained the crustal thickness is about 37 km with VP/Vs ratio 2.2 beneath station SOEI. We suggest that the high Vp/Vs in station PLAI may indicate the presence of fluid ascending from the subducted plate to the volcanic arc, whereas the high Vp/Vs in station SOEI could be due to the presence of sediment and rich mafic composition in the upper crust and possibly related to the serpentinization process in the lower crust. We also suggest that the difference in velocity models and crustal thicknesses between stations PLAI and SOEI are consistent with their contrasting tectonic environments.},
doi = {10.1063/1.4915016},
journal = {AIP Conference Proceedings},
issn = {0094-243X},
number = 1,
volume = 1658,
place = {United States},
year = {2015},
month = {4}
}