Titlebook: Seismicity Associated with Mines, Reservoirs and Fluid Injections; Shahriar Talebi Conference proceedings 1998 Springer Basel AG 1998 Rese

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978-3-7643-5878-5Springer Basel AG 1998

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An Anatomy of a Seismic Sequence in a Deep Gold Mine,hest value of . = 2.4, whereas the third and fourth sequences are characterized by the middle value of .= 1.9..The corner frequencies of . and . waves are in close proximity and range from 14 to 220 Hz. A display of source parameters as a function of time shows that the four main shocks are most dis

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On the Nature of Reservoir-induced Seismicity,ry results of two-dimensional (similar to those by ., 1988) calculations suggest that, this “protracted seismicity” depends on the frequency and amplitude of lake-level changes, reservoir dimensions and hydromechanical properties of the substratum. Strength changes show delays with respect to lake-l

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Seismicity around Dhamni Dam, Maharashtra, India,e months of January–February and August–September. Seismicity has continued at a low level during 1995 and 1996. The hypocenters are located in a volume of 10 × 10 × 10 km. situated just south of the reservoir along the NW trending Kalu-Surya fault. Correlation of a space-time pattern of seismicity