About: Detection of high-frequency tensile vibrations of a fault during shear rupturing: observations from the 2008 West Bohemia swarm     Goto   Sponge   NotDistinct   Permalink

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  • The analysis of 12 earthquakes of magnitudes between 1.7 and 3.7 that occurred in 2008 in West Bohemia, Czech Republic reveals that shear rupturing along a fault is accompanied by weak tensile vibrations of the fault. The vibrations are of a narrow frequency band with frequencies distinctly higher than those of shear rupturing. The tensile vibrations decay slowly in time and often resemble resonant waves. They complicate the radiated P waveforms and the P-wave radiation pattern. The tensile vibrations can be observed in waveforms in directions near the nodal lines where the dominance of shear-faulting radiation is lost. The tensile vibrations are probably generated by opening of the fault during shear rupturing or by creating a wing tensile crack at the tip of the fault when shear fracturing stops.
  • The analysis of 12 earthquakes of magnitudes between 1.7 and 3.7 that occurred in 2008 in West Bohemia, Czech Republic reveals that shear rupturing along a fault is accompanied by weak tensile vibrations of the fault. The vibrations are of a narrow frequency band with frequencies distinctly higher than those of shear rupturing. The tensile vibrations decay slowly in time and often resemble resonant waves. They complicate the radiated P waveforms and the P-wave radiation pattern. The tensile vibrations can be observed in waveforms in directions near the nodal lines where the dominance of shear-faulting radiation is lost. The tensile vibrations are probably generated by opening of the fault during shear rupturing or by creating a wing tensile crack at the tip of the fault when shear fracturing stops. (en)
Title
  • Detection of high-frequency tensile vibrations of a fault during shear rupturing: observations from the 2008 West Bohemia swarm
  • Detection of high-frequency tensile vibrations of a fault during shear rupturing: observations from the 2008 West Bohemia swarm (en)
skos:prefLabel
  • Detection of high-frequency tensile vibrations of a fault during shear rupturing: observations from the 2008 West Bohemia swarm
  • Detection of high-frequency tensile vibrations of a fault during shear rupturing: observations from the 2008 West Bohemia swarm (en)
skos:notation
  • RIV/67985530:_____/11:00363813!RIV12-AV0-67985530
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300120801), Z(AV0Z30120515)
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  • 3
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  • 193710
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  • RIV/67985530:_____/11:00363813
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • earthquake dynamics; earthquake source observations; body waves; dynamics and mechanics of faulting (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [F3391CFC5B6D]
http://linked.open...i/riv/nazevZdroje
  • Geophysical Journal International
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  • 186
http://linked.open...iv/tvurceVysledku
  • Vavryčuk, Václav
http://linked.open...ain/vavai/riv/wos
  • 000293998000036
http://linked.open...n/vavai/riv/zamer
issn
  • 0956-540X
number of pages
http://bibframe.org/vocab/doi
  • 10.1111/j.1365-246X.2011.05122.x
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