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Mining Induced Seismicity

๐Ÿ“„๏ธ Grid Based Analysis

The Grid Based Analysis application can be used to evaluate the spatial distribution of various seismic parameters. There are a range of source parameter options available, and they can give indications to the rock mass behaviour. Some parameters can be considered as a proxy (stand-in) for rock mass stress, while other parameters can be a proxy for the amount of deformation. There are also parameters available that are associated with the rock mass mechanism or event type.

๐Ÿ“„๏ธ Hazard Assessment - Event Rate

The Hazard Assessment application uses a grid-based approach to describe the seismic hazard throughout your mine. Each grid point essentially represents a seismic source with a specific frequency-magnitude relationship. A frequency-magnitude relationship is defined from the $M$, $Mmin$, $b$-value, and event rate. We've previously delved into $M{UL}$ in this post. We also discussed how $Mmin$ and $b$-value are calculated along with other gridding parameters in this post. The event rate is something we haven't taken a dive into yet, so we'll get into it in this post.

๐Ÿ“„๏ธ Stochastic declustering explained

As mentioned in the last blog post, a stochastic declustering algorithm has been implemented in mXrap to separate events into 'clustered' and 'background' components. It can be useful when designing seismic exclusions and re-entry procedures to separate seismicity that occurs in short bursts from seismicity that has low variability in space and time. Short-term exclusions cannot be used to manage the risk associated with background seismicity, since the hazard inside a potential exclusion would be the same as outside the exclusion. Efficient exclusion and re-entry procedures target areas where seismicity is most clustered and where the seismic hazard to which people are exposed can be reduced with a short disruption to production.