By Renata Dmowska (ed.), Barry Saltzman (ed.)
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Extra resources for Advances in Geophysics, Vol. 32
84-07-12 H=O 1 K M 3 bt 0 , 2 8 43 - 0 70 - 12 ' R T. 67N S O L U T I O N 16 a M-0 9. 84-07-21 0 KM b M = O 5. 63 5 W FIG. 15. Alternative fault-plane solutions for seismic events with all dilatational (open circles) P-wave first motions, recorded in the East Mountain coal mining area, Wasatch Plateau, Utah during June- August 1984. Lower hemisphere, equal-area projections are used. Triangles indicate P- and Faxes and alternative slip vectors; H is the focal depth and M is magnitude. 6 km below datum.
01 MPa. A high stress-drop event is very often represented by a simple pulse with a welldefined corner frequency and relatively steep high-frequency fall-off, whereas many of the low stress drop events are more complex, in both the time and frequency domains. Recently McGarr et al. (1989) presented the results of their analysis of large mine tremors in two gold mining districts of South Africa. In the Klerksdorp district, where the strata are offset by major normal faults, the largest tremors tend to be associated with slip on these preexisting faults, their source size is large and the stress drop is low.
The linear programming moment-tensor inversion (Julian, 1986) provides the most powerful technique for the investigation of the range of possible source mechanisms consistent with a particular set of first-motion or amplitude data. In the frequency domain the vector u in the system of Eqs. (1) is replaced by the low-frequency spectral level of displacement, which can then be normalized by the transfer function for each station for geometrical spreading, attenuation, and the effect of the crust including the free surface; and the excitation matrix for P, S H , or SV waves is taken into account.
Advances in Geophysics, Vol. 32 by Renata Dmowska (ed.), Barry Saltzman (ed.)