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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F11%3A00363813%21RIV12-AV0-67985530
rdf:type
skos:Concept n9:Vysledek
dcterms:description
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.
dcterms: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
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
skos:notation
RIV/67985530:_____/11:00363813!RIV12-AV0-67985530
n9:predkladatel
n10:ico%3A67985530
n5:aktivita
n12:Z n12:P
n5:aktivity
P(IAA300120801), Z(AV0Z30120515)
n5:cisloPeriodika
3
n5:dodaniDat
n8:2012
n5:domaciTvurceVysledku
n14:4755405
n5:druhVysledku
n19:J
n5:duvernostUdaju
n11:S
n5:entitaPredkladatele
n15:predkladatel
n5:idSjednocenehoVysledku
193710
n5:idVysledku
RIV/67985530:_____/11:00363813
n5:jazykVysledku
n17:eng
n5:klicovaSlova
earthquake dynamics; earthquake source observations; body waves; dynamics and mechanics of faulting
n5:klicoveSlovo
n6:earthquake%20dynamics n6:earthquake%20source%20observations n6:dynamics%20and%20mechanics%20of%20faulting n6:body%20waves
n5:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n5:kontrolniKodProRIV
[F3391CFC5B6D]
n5:nazevZdroje
Geophysical Journal International
n5:obor
n13:DC
n5:pocetDomacichTvurcuVysledku
1
n5:pocetTvurcuVysledku
1
n5:projekt
n18:IAA300120801
n5:rokUplatneniVysledku
n8:2011
n5:svazekPeriodika
186
n5:tvurceVysledku
Vavryčuk, Václav
n5:wos
000293998000036
n5:zamer
n16:AV0Z30120515
s:issn
0956-540X
s:numberOfPages
11
n20:doi
10.1111/j.1365-246X.2011.05122.x