Comparison of P-Wave Tomography Model in Sunda-Banda Arc by Using Data from BMKG and ISC. Issue 1 (October 2021)

• Record Type: Journal Article
• Authors: Brilianti, P T; Haq, M S; Haolia, ; Sulaiman, M I; Nugroho, R P; Oka, A S B; Pranowo, W; Suhardja, S K; Nugraha, A D; Zulfakriza, Z; Widiyantoro, S; Ramdhan, M
• Is Part Of: IOP conference series. Volume 873:Issue 1(2021)
• Publication Date: 2021-10
• Subjects: Sunda-Banda Arc -- Back Arc Thrust -- FMTOMO; Earth sciences -- Periodicals; Environmental sciences -- Congresses; Environmental sciences -- Periodicals; 550.5
• DOI: 10.1088/1755-1315/873/1/012058
• Languages: English
• ISSNs: 1755-1307

Abstract

Abstract: The tectonic setting of our study area is located between the Island of Java and Timor Leste. The complexity of this region is started with two different plates, The Indo-Australian plate and the Eurasian plate that move with different orientations and convergence rate. This area also shows active seismic activity and has a series of active volcanoes as a product of subduction and collision. To deepen understand this area, we perform delay time tomography using FMTOMO package that includes 3-D finite-difference based ray tracing and sub-space inversion procedure. We used two different sets of data, the first one is 4 years data catalog from the Indonesian Agency of Meteorology, Climatology and Geophysics, and the second one is 47 years of data from the International Seismological Centre. Data from the local Indonesian show agency shows a fewer number of events but more focus clusters. Meanwhile, the data from ISC catalog has more events and evenly distributed data. However, we also noticed that data from ISC has cluster events located at the same depth that can be improved with events relocation for better depth estimation. The Checkerboard models from both data set show a comparable result, though data from ISC show a better recovered model at a deeper depth and shallow part in the eastern area. The checkerboard from the local Agency shows slightly better results in the shallow part. Next, we invert delay time for each data set using we optimized damping and smoothing parameters. Final tomogram models show that data from the local Agency show a more continuous fast velocity band representing a downgoing subducting slab and possible back-arc thrust while results from the ISC data show a more detached fast velocity band that could be contributed from fixed depth problem in the data set. However, we noticed that data from ISC show a higher amplitude low-velocity anomaly especially in the shallow depth