Structure and seismic signature of subsidiary damage around natural and artificial fractures
The observed fractal nature of both fault length distributions and earthquake magnitude-frequency distributions suggests that there may be a direct relationship between the structure of active fault systems and the resulting seismicity. In much previous theoretical work, a positive correlation betwe...
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University of Edinburgh
1992
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.652229 |