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Source Characteristics of the 28 September 2018 Mw 7.5 Palu-Sulawesi, Indonesia (SE Asia) Earthquake Based on Inversion of Teleseismic Bodywaves

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Abstract

We study source characteristics of the September 28, 2017 Mw 7.5 Palu (Sulawesi, Indonesia) earthquake that occurred in central Sulawesi and triggered devastating tsunami waves along the coastal plains of the island. We apply point-source teleseismic P- and SH-body waveform inversion and kinematic slip inversion techniques to obtain double-couple source mechanism and comprehensive finite-fault slip model of the source. The overall results show a strike-slip faulting mechanism (strike: 353° ± 5°, dip: 65° ± 5° and rake angles: − 4° ± 5°) with a small amount of dip-slip component at a shallow focal depth of 16 ± 2 km associated with the NW–SE trending left-lateral Palu-Koro strike-slip fault in the central Sulawesi region. The P- wave first motion polarity readings recorded at near-field and regional seismic stations are found to be reasonably consistent with the source mechanism solution of the earthquake and estimated error limits. We have extensively studied and considered the rupture velocity to be about 4.1 km/s during the slip inversion as previously proposed by seismological and geodetic studies for this event. The obtained finite-fault slip distribution model displays a rupture starting from the hypocentre located at 16 km, and then it propagated south accompanied by high amount of displacement, and reached the surface. The model has two slip-patches of 2.0–4.0 m at north of the fault plane, and 5.0–6.3 m at south near Palu city, which is very well matched with the observed damage and destruction related to the earthquake. The fault length and width, average slip and stress drop values are estimated to be 150 km, 45 km, 1.5 m and 13 bars, respectively. We have also obtained total source duration to be about 40 s with the most of seismic energy released at 10 s and 25 s. Furthermore, a small dip-slip component is evidently observed from both source models, and we suggest that this oblique shear which reflects the bending of slip vector along the strike direction could be comparatively responsible for tsunami generation along the left-lateral Palu-Koro Fault. The validation of this hypothesis could be done by evaluating the results of the mathematical tsunami simulations based on the comprehensive non-uniform slip models along with a high-resolution bathymetry data, which provides the details of the continental shelf in Palu bay.

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Acknowledgements

We would like to thank Turkish Academy of Sciences (TÜBA) in the framework for Young Scientist Award Program (TÜBA-GEBIP), İstanbul Technical University Research Fund (İTÜ-BAP), Turkish National Scientific Technological Foundation (TÜBİTAK), and Alexander von Humboldt Foundation (AvH) for their financial support. Teleseismic body waveform data used are from the International Federation of Digital Seismograph Networks (FDSN) and the Global Digital Seismograph Network (GDSN) stations and archived at the IRIS-DMC, http://ds.iris.edu/wilber3. The Generic Mapping Tools (GMT; Wessel and Smith 1998) and SAC2000 software packages (Goldstein et al. 2003; Goldstein and Snoke 2005) were used for the preparation of the figures and for processing conventional earthquake data, respectively. We appreciate Yuji Yagi’s generous permission to use the kinematic slip inversion code to analyze rupture history and slip distribution models. We also thank two anonymous reviewers and Alexander Rabinovich (Editor-in-Chief) for their constructive comments and suggestions which have improved this manuscript.

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  1. Geophysical Engineering Department, The Faculty of Mines, İstanbul Technical University, Maslak, 34469, Istanbul, Turkey

    Seda Yolsal-Çevikbilen & Tuncay Taymaz

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  1. Seda Yolsal-Çevikbilen
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Yolsal-Çevikbilen, S., Taymaz, T. Source Characteristics of the 28 September 2018 Mw 7.5 Palu-Sulawesi, Indonesia (SE Asia) Earthquake Based on Inversion of Teleseismic Bodywaves. Pure Appl. Geophys. 176, 4111–4126 (2019). https://doi.org/10.1007/s00024-019-02294-1

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