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. 2016 Nov 9;6:36676. doi: 10.1038/srep36676

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Copyright © 2016, The Author(s)

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(a) Normalised source-time history (slip on the fault). (b) Moment-rate spectrum fit with a ω²-source model²⁸. The flat part of the spectrum (left arrow) corresponds to the seismic moment M₀, while the corner frequency f_c (right arrow) is related to the source size. The results shown are calculated for V_P = 500 m/s and ν = 0.3 and the source location from Fig. 3b. Note that varying ν between 0.25 and 0.35 does not affect the corner frequency to a large extent (f_c = 4.2–5.6 Hz).