Slope stability monitoring from microseismic field using polarization methodology; Natural Hazards and Earth System Sciences (NHESS); Vol. 3, iss. 6
| Parent link: | Natural Hazards and Earth System Sciences (NHESS) Vol. 3, iss. 6.— 2003.— [P. 515-521] |
|---|---|
| Outros autores: | , , , |
| Summary: | Title screen Numerical simulation of seismoacoustic emission (SAE) associated with fracturing in zones of shear stress concentration shows that SAE signals are polarized along the stress direction. The proposed polarization methodology for monitoring of slope stability makes use of three-component recording of the microseismic field on a slope in order to pick the signals of slope processes by filtering and polarization analysis. Slope activity is indicated by rather strong roughly horizontal polarization of the respective portion of the field in the direction of slope dip. The methodology was tested in microseismic observations on a landslide slope in the Northern Tien-Shan (Kyrgyzstan). |
| Idioma: | inglés |
| Publicado: |
2003
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| Subjects: | |
| Acceso en liña: | http://www.nat-hazards-earth-syst-sci.net/3/515/2003/nhess-3-515-2003.html |
| Formato: | Electrónico Capítulo de libro |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=638956 |
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| 200 | 1 | |a Slope stability monitoring from microseismic field using polarization methodology |f Yu. I. Kolesnikov [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 330 | |a Numerical simulation of seismoacoustic emission (SAE) associated with fracturing in zones of shear stress concentration shows that SAE signals are polarized along the stress direction. The proposed polarization methodology for monitoring of slope stability makes use of three-component recording of the microseismic field on a slope in order to pick the signals of slope processes by filtering and polarization analysis. Slope activity is indicated by rather strong roughly horizontal polarization of the respective portion of the field in the direction of slope dip. The methodology was tested in microseismic observations on a landslide slope in the Northern Tien-Shan (Kyrgyzstan). | ||
| 461 | |t Natural Hazards and Earth System Sciences (NHESS) | ||
| 463 | |t Vol. 3, iss. 6 |v [P. 515-521] |d 2003 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 701 | 1 | |a Kolesnikov |b Yu. I. | |
| 701 | 1 | |a Nemirovich-Danchenko |b M. M. |c geophysicist |c Professor of Tomsk Polytechnic University, Doctor of physical and mathematical sciences |f 1955- |g Mikhail Mikhailovich |3 (RuTPU)RU\TPU\pers\32898 | |
| 701 | 1 | |a Goldin |b S. V. | |
| 701 | 1 | |a Seleznev |b V. S. | |
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| 856 | 4 | |u http://www.nat-hazards-earth-syst-sci.net/3/515/2003/nhess-3-515-2003.html | |
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