Abstract
<jats:p>Source parameters such as seismic moment, corner frequency, stress drop, radiated energy, and apparent stress are often derived from the Brune (1970) source spectrum. Building on this, Andrews (1986) formulated analytical relations that link those parameters to spectral integrals of squared velocity and displacement, and Snoke (1987) introduced an approximation that enables their practical estimation from limited- band data. However, subsequent studies have adopted inconsistent numerical coefficients in Snoke’s expression for the low-frequency spectral level. Our rederivation confirms that the correct coefficient is 2, rather than 4^(1/4), and shows that the discrepancy arises from a computational oversight in the original formulation. We further clarify how Snoke’s integral approximation extends to radiated energy and apparent stress, highlighting the linkage between inferred source parameters, dynamic rupture process, and energy balance. This re-examination would support consistent use of spectral formulations in earthquake source parameter estimation and underscore the need for caution when estimating and interpreting source parameters, especially secondary quantities.</jats:p>