Resumo

BRANDT, M.B.C.. Near-surface wave attenuation (kappa) of Far West Rand micro-events. J. S. Afr. Inst. Min. Metall. [online]. 2017, vol.117, n.6, pp.511-516. ISSN 2411-9717.  http://dx.doi.org/10.17159/2411-9717/2017/v117n6a1.

The near-surface wave attenuation factor k (kappa), which describes the attenuation of seismic waves with distance in the upper 1-3 km of the Earth, was determined for the Far West Rand gold mining area using seismic data recorded by station Parys (PRYS) of the South African National Seismograph Network. Twenty micro-events in the magnitude range 0.7 < M_L< 1.8 for the period 1 July to 15 November 2015 were analysed. For the analysis a 10-second window for the S phase portion of the vertical component seismogram was selected. The result was an average k = 0.048 ± 0.014 s, which is much higher than for a stable continental region where k ≈ 0.006 s. This is because the assumed Brune source model is inappropriate for describing mining-related events that often have moment tensors with a volumetric (implosive) component. The average k was calculated to be 0.098 ± 0.038 s for explosions of a similar magnitude. This higher value derived for mining-related k may be employed as a means of correcting the Brune source spectrum to calculate seismic moment as well as corner frequency for events in the mining areas of South Africa.

Palavras-chave : Kappa; near-surface attenuation; mining-related seismic event; spectral analysis.

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