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  • The earthquake source mechanism (description of the geometry of the source and its strength in terms of forces equivalent to rupturing of the rock mass) is routinely modeled as a moment tensor (MT) describing the earthquake focus as a point. However, sometimes this approximation is not satisfied, and seismic radiation keeps the directivity due to the finite extent of the source. Inversion into the MT then may yield a biased mechanism. Synthetic study in the Adamová and Šílený (2010) demonstrated the appearance of spurious non-double-couple components in the mechanism even for a pure double-couple (DC) source. Their method was designed to reduce the spurious source components by using the second-degree moments to evaluate their contribution into the records and subtract it from the data. Here we applied the procedure to five moderate to large regional events with large nonshear components. They are mostly located on large tectonic faults where predominantly pure shear slip is expected. We studied one event on the prominent North Anatolian fault, three events in the Pacific area, and one event in Bolivia.
  • The earthquake source mechanism (description of the geometry of the source and its strength in terms of forces equivalent to rupturing of the rock mass) is routinely modeled as a moment tensor (MT) describing the earthquake focus as a point. However, sometimes this approximation is not satisfied, and seismic radiation keeps the directivity due to the finite extent of the source. Inversion into the MT then may yield a biased mechanism. Synthetic study in the Adamová and Šílený (2010) demonstrated the appearance of spurious non-double-couple components in the mechanism even for a pure double-couple (DC) source. Their method was designed to reduce the spurious source components by using the second-degree moments to evaluate their contribution into the records and subtract it from the data. Here we applied the procedure to five moderate to large regional events with large nonshear components. They are mostly located on large tectonic faults where predominantly pure shear slip is expected. We studied one event on the prominent North Anatolian fault, three events in the Pacific area, and one event in Bolivia. (en)
Title
  • Disputable non-double-couple mechanisms of several strong earthquakes: second-degree moment approach
  • Disputable non-double-couple mechanisms of several strong earthquakes: second-degree moment approach (en)
skos:prefLabel
  • Disputable non-double-couple mechanisms of several strong earthquakes: second-degree moment approach
  • Disputable non-double-couple mechanisms of several strong earthquakes: second-degree moment approach (en)
skos:notation
  • RIV/67985530:_____/13:00396790!RIV14-GA0-67985530
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GAP210/10/0296)
http://linked.open...iv/cisloPeriodika
  • 5
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 69918
http://linked.open...ai/riv/idVysledku
  • RIV/67985530:_____/13:00396790
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Izmit Turkey earthquake; 1995 Kobe earthquake; rupture processes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [CDA371E700BE]
http://linked.open...i/riv/nazevZdroje
  • Bulletin of the Seismological Society of America
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 103
http://linked.open...iv/tvurceVysledku
  • Šílený, Jan
  • Adamová, Petra
http://linked.open...ain/vavai/riv/wos
  • 000324986700021
issn
  • 0037-1106
number of pages
http://bibframe.org/vocab/doi
  • 10.1785/0120130014
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