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Result

Probabilistic Aftershock Hazard Assessment I: Numerical Testing of Methodological Features

Probabilistic Aftershock Hazard Assessment I: Numerical Testing of Methodological Features...

DC - Seismologie, vulkanologie a struktura Země

  • 2008
  • Jx
Result

Probabilistic Aftershock Hazard Assessment II: Application of Strong Ground Motion Modeling

Probabilistic Aftershock Hazard Assessment II: Application of Strong Ground Motion Modeling...

DC - Seismologie, vulkanologie a struktura Země

  • 2008
  • Jx
Result

Aftershocks triggered by fluid intrusion: Evidence for the aftershock sequence occurred 2014 in West Bohemia/Vogtland

overlapping with previous swarm activity, consisted of three classical aftershock change from swarm-type to mainshock-aftershock characteristics, we have analyzed field. Most of its intense aftershock activity occurred in-...

DC - Seismologie, vulkanologie a struktura Země

  • 2016
  • Jx
  • Link
Result

Aftershock monitoring of the Athens earthquake of September 7, 1999

Aftershock monitoring of the Athens earthquake of September 7, 1999...

DC - Seismologie, vulkanologie a struktura Země

  • 2000
  • Jx
Result

Internal tectonic structure of the Central American Wadati-Benioff zone based on analysis of aftershock sequences

Internal tectonic structure of the Central American Wadati-Benioff zone based on analysis of aftershock sequences...

DE - Zemský magnetismus, geodesie, geografie

  • 2007
  • Jx
Result

Linear Relationship Between Aftershock Productivity and Seismic Coupling in the Northern Chile Subduction Zone

The aftershock productivity is known to strongly vary for different mainshocks Chile, that the aftershock productivity is linearly related to the degree, we show that the observed aftershock numbers are significantly lower ...

Volcanology

  • 2019
  • Jimp
  • Link
Result

Probing the northern Chile megathrust with seismicity: The 2014 M8.1 Iquique earthquake sequence

detected and located 19,000 foreshocks, aftershocks, and background seismicity for 1 the updip limit of the mainshock asperity, aftershocks occur mainly in two belts updip to the mainshock and its largest aftershock. After...

Volcanology

  • 2019
  • Jimp
  • Link
Result

Resolution of non-double-couple components in the seismic moment tensor using regional networks-II: application to aftershocks of the 1999 M-w 7.4 Izmit earthquake

We study potential non-double-couple (non-DC) components in aftershocks mechanisms of Izmit aftershocks clearly indicate a segmentation of the rupture coverage, we applystrict quality criteria to the aftershock catalogue re...

DC - Seismologie, vulkanologie a struktura Země

  • 2014
  • Jx
  • Link
Result

Simulation of aftershock series.

Annotation not available...

DB - Geologie a mineralogie

  • 1994
  • Jx
Result

Simulation of aftershock series from rock samples

DC - Seismologie, vulkanologie a struktura Země

  • 1994
  • Jx
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