Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/14822
Title: New Insights into the Source of the Makran Tsunami of 27 November 1945 from Tsunami Waveforms and Coastal Deformation Data
Authors: Heidarzadeh, M
Satake, K
Keywords: Makran earthquake of 27 November 1945;Tsunami;Makran subduction zone;Spectral analysis;Fourier analysis;Wavelet analysis;Tsunami waveform inversion;Co-seismic deformation
Issue Date: 2014
Citation: Pure and Applied Geophysics, 2015, 172 (3-4), pp. 621 - 640
Abstract: © 2014, Springer Basel.We constrain the source of the 27 November 1945 tsunami in the Makran Subduction Zone (MSZ) using available tsunami waveforms recorded on tide gauges at Mumbai (India) and Karachi (Pakistan), and that inferred at Port Victoria (Seychelles), and coseismic deformation data along the Makran coast. Spectral analysis of the tsunami waveforms shows that the tsunami governing period was 40–50 min at Karachi whereas it was around 22 min at Mumbai. The inferred tsunami waveform at Port Victoria also indicated a period of around 21 min for the tsunami. Tsunami numerical simulations from the previously proposed source models failed in reproducing the observed tsunami waveforms and coseismic deformation data. Sensitivity analysis showed that the source fault needs to be extended offshore into deep water in order to reproduce the first 22-min signal at Mumbai. Based on the inversion of the observed tsunami waveforms, we propose a four-segment fault with varying slip amounts as the final source. This source includes a slip of 4.3 m onshore near Ormara (Pakistan) and a slip of 10 m offshore at water depth of around 3,000 m. The total fault length is 220 km, and the average slip is 6.1 m. This source, first, reproduces fairly well the observed tide gauge records at Mumbai and Karachi, second, produces ~1 m of uplift at Ormara and ~1 m of subsidence at Pasni, and third, gives a moment magnitude of 8.3 for the earthquake, which is in the acceptable range of seismic data. The computed 1 m uplift at Ormara is in the uplift range of 1–3 m reported in the literature. As the tide gauge stations were located in the far field, our proposed source explains mainly the tectonic source of the tsunami.
URI: http://bura.brunel.ac.uk/handle/2438/14822
DOI: http://dx.doi.org/10.1007/s00024-014-0948-y
ISSN: 0033-4553
1420-9136
Appears in Collections:Dept of Mechanical Aerospace and Civil Engineering Research Papers

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