2008
DOI: 10.1007/s10913-008-0038-6
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Anomalies of low-intensity acoustic wave attenuation in rocks

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Cited by 5 publications
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“…When the fracture reaches approximately half its breaking strength, a range of crevasses starts to appear and produces high energy level AE called "microseisms. " To a certain extent, the intensity and frequency of microseisms and AE reflect the stress state and deformation energy release rate of a coal rock mass [1][2][3][4][5]. The monitoring of microseisms began in the 1990s.…”
Section: Introductionmentioning
confidence: 99%
“…When the fracture reaches approximately half its breaking strength, a range of crevasses starts to appear and produces high energy level AE called "microseisms. " To a certain extent, the intensity and frequency of microseisms and AE reflect the stress state and deformation energy release rate of a coal rock mass [1][2][3][4][5]. The monitoring of microseisms began in the 1990s.…”
Section: Introductionmentioning
confidence: 99%