We determine the seismic moment and corner frequency of earthquakes using narrowband, time‐domain measurements of the maximum shear‐wave displacement amplitude. Each S wave is passed through a set of one‐octave band‐pass filters between 0.25 and 32 Hz to measure the peak amplitude on the horizontal components. Following the development of Richter (1935) local magnitude scale, we derive a functional form of maximum amplitude versus distance, but separately for each frequency band, and use them to estimate wave attenuation as a function of frequency and distance. Attenuation is a strong function of frequency, approximately proportional to 1/f⁠, with path averaged Q increasing (attenuation decreasing) with propagation distance. We use these empirical attenuation curves to correct the time‐domain peak amplitudes to a reference distance of 10 km to recover the source spectrum. We find that the spectral shape is consistent with the Brune model, showing a well‐defined plateau at low frequency and a decay at high frequency proportional to ω−2⁠. We use the median spectrum for stations at distances up to 120 km for each event to measure the moment and corner frequency. This time‐domain method provides a reliable and efficient way to accurately measure earthquake source parameters.

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