We applied the magnitude determination method of Hara (2007a, b) to
the September 24, 2013 63 km NNE of Awaran, Pakistan earthquake
(the origin time: 11:29:47 UTC; the location 26.971N 65.520E depth=15.0km after USGS).
In this method, an earthquake magnitude, M, is calculated by the following formula:
Fig. 1. An example of measurements of high frequency energy radiation. The upper, middle and lower traces are an observed seismogram, the squares of the band-pass (2-4 Hz) filtered seismogram, and its smoothed time series (normalized by the maximum value), respectively. gAh and gFh in the lower trace denote the arrival of P-wave and estimated end of high frequency energy radiation, respectively.
Acknowledgements
We retrieved BHZ channel waveform data, recorded at the Global Seismograph Network (GSN)
stations, from IRIS DMC (Incorporated Research Institutions for Seismology,
Data Management Center). We used SAC (Seismic Analysis Code) (Goldstein et al., 2007)
for seismic waveform data analyses.
References
This analysis was done by Tatsuhiko Hara.
Last Updated: 2013/09/26