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Bulletin of the Seismological Society of America; October 1971; v. 61; no. 5; p. 1453-1466
© 1971 Seismological Society of America
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Violent deformation of rock near deep-level, tabular excavations—seismic events

ARTHUR MCGARR

BERNARD PRICE INSTITUTE OF GEOPHYSICAL RESEARCH UNIVERSITY OF THE WITWATERSRAND, JOHANNESBURG, South Africa

Abstract

Inelastic deformation of the rock near the edges of the thin tabular excavations (stopes) of deep-level mines sometimes occurs violently, resulting in a seismic event. These seismic events are produced in the highly-stressed rock near the edges of the stopes and appear to be the result of shear failure across a plane; these conclusions are based on seismic as well as underground observations.

The seismic events occurring near stopes can be described using a model based on the theory of dislocations; they result from two edge dislocations of opposite sign annihilating each other and releasing energy. The instantaneous convergence of the stope that is observed to occur at the time of a large mine tremor is compatible with the observed seismic energy of the tremor, according to analysis based on the dislocation model.




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