Abstract
In this chapter, I will be comparing seismicity recorded in the Diablo Regimento hydro-fractured cave with the seismicity recorded in the two non-preconditioned caves of PMC and DOZ. For comparison between mines, I will be using cave volumes. At Diablo Regimento Sector, the cave volume that will was used is the volume that was reconditioned with the hydro-fracturing technique. Analysis of the seismicity recorded in the three caves presented in this chapter leads to a number of conclusions. The most important one is that the preconditioning of the DR rock mass had to result in substantial fracturing of the rock mass. A similar rock mass condition to what was already in place at DR right from the commencement of the cave mining , was achieved only after nearly 3 years of production at PMC. The PMC rock mass was gradually preconditioned by the caving process.
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Gibowicz SJ, Kijko A (1994) An introduction to mining seismology. Academic Press, New York
Glazer SN (2016) Mine seismology: data analysis and interpretation. Palabora mine caving process as revealed by induced seismicity. Springer International Publishing, Switzerland (ISBN 978-3-319-32611-5)
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Glazer, S.N. (2019). Comparison of Seismicity Induced While Mining Hydro-fractured and Non-preconditioned Rock Mass Volumes. In: Mine Seismology: Seismic Response to the Caving Process. Springer, Cham. https://doi.org/10.1007/978-3-319-95573-5_4
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DOI: https://doi.org/10.1007/978-3-319-95573-5_4
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