2020
DOI: 10.1093/gji/ggaa449
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Application of a convolutional neural network for seismic phase picking of mining-induced seismicity

Abstract: Summary Monitoring mining-induced seismicity (MIS) can help engineers understand the rock mass response to resource extraction. With a thorough understanding of ongoing geomechanical processes, engineers can operate mines, especially those mines with the propensity for rockbursting, more safely and efficiently. Unfortunately, processing MIS data usually requires significant effort from human analysts, which can result in substantial costs and time commitments. The problem is exacerbated for oper… Show more

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Cited by 29 publications
(8 citation statements)
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“…There has been some application of TL to seismology (e.g., Chai et al 2020, Titos et al 2019, Johnson et al 2021, Otović et al 2021) although its use is not yet widespread for applications of ML in seismology. In this study, we explore the use of TL for improving our IM prediction algorithm.…”
Section: Introductionmentioning
confidence: 99%
“…There has been some application of TL to seismology (e.g., Chai et al 2020, Titos et al 2019, Johnson et al 2021, Otović et al 2021) although its use is not yet widespread for applications of ML in seismology. In this study, we explore the use of TL for improving our IM prediction algorithm.…”
Section: Introductionmentioning
confidence: 99%
“…(3) After the initial breakage of the hard-thick strata, periodic breakage of the hard-thick strata will occur as the 221 upper 03 working face continues to advance. According to the calculation of "cantilever beam" structure [27][28] , the periodic breakage distance of the hard-thick strata is 25 m. In other words, the periodic breakage of the hard-thick strata will occur when the working face advances at least 138 m, and the cycle will continue until the end of the working face, as shown in Figure 5.…”
Section: Fracture Mechanism Of Hard-thick Rock Stratamentioning
confidence: 99%
“…Mining-triggered tremors exhibit characteristic features that distinguish them from natural earthquakes. The differences relate mainly to the mechanism of shock generation, the wave propagation from the source to the receiver, the range of dominant frequencies, duration, and repeatability of occurrence [18][19][20]. In a typical record of mining-triggered vibrations [21], in close proximity to the source, amplitudes of vertical oscillations are comparable to or even higher than amplitudes of horizontal vibrations.…”
Section: Introductionmentioning
confidence: 99%