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  1. Acta Geodaetica et Geophysica Hungarica
  2. Acta Geodaetica et Geophysica Hungarica : Volume 43
  3. Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 2-3, June 2008
  4. Ground motion models — State of the art
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Acta Geodaetica et Geophysica Hungarica : Volume 52
Acta Geodaetica et Geophysica Hungarica : Volume 51
Acta Geodaetica et Geophysica Hungarica : Volume 50
Acta Geodaetica et Geophysica Hungarica : Volume 49
Acta Geodaetica et Geophysica Hungarica : Volume 48
Acta Geodaetica et Geophysica Hungarica : Volume 47
Acta Geodaetica et Geophysica Hungarica : Volume 46
Acta Geodaetica et Geophysica Hungarica : Volume 45
Acta Geodaetica et Geophysica Hungarica : Volume 44
Acta Geodaetica et Geophysica Hungarica : Volume 43
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 4, December 2008
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 2-3, June 2008
Preface
Evidence of strong lateral inhomogeneous structure beneath SE Carpathians and specific mantle flow patterns
Spatial and temporal variations of the correlation coefficient between M2 and S2 earth tides components and earthquake occurrences for the intermediate-depth seismic activity zones
Romanian Seismic Network development
Review of the historical seismicity in the western and southwestern territory of Romania (Banat Seismic Region)
Seismicity patterns in Vrancea and predictive features
Inversion of the October 27, 2004 Vrancea (Romania) earthquake using teleseismic waveforms data
Thermal models simulating the tectonic processes in the extra-Carpathian area (on the Romanian territory): rheological models and their interpretation in relation with the local seismic wave attenuation models
Seismotectonic modeling for seismic hazard analysis of Vardar zone in Republic of Macedonia
Evaluation of PGA for Tirana city
Analysis of strong motion data from three events (M $_{W}$ = 4.3–4.9) recorded recently in central Albania area
An approach of Microzonation of the Sofia city
Estimation of an upper limit on prehistoric peak ground acceleration using the parameters of intact speleothems in caves situated at the western part of Balkan Mountain Range, North-West Bulgaria
Ground motion models — State of the art
History of early isoseismal maps
Fragility evaluation of existing typified school buildings in Albania
Some remarks on the seismic risk to lifelines, with references to the activity of the Vrancea seismogenic zone
Seismic safety of structures — Case study: Probabilistic methodological approach to definition of seismic input
Synthesis of nonstationary seismic response of structures
Simulation and analysis of seismic response of a structure for Sofia region with synthetic accelerograms
Acta Geodaetica et Geophysica Hungarica : Volume 43, Issue 1, March 2008
Acta Geodaetica et Geophysica Hungarica : Volume 42
Acta Geodaetica et Geophysica Hungarica : Volume 41
Acta Geodaetica et Geophysica Hungarica : Volume 40
Acta Geodaetica et Geophysica Hungarica : Volume 39
Acta Geodaetica et Geophysica Hungarica : Volume 38
Acta Geodaetica et Geophysica Hungarica : Volume 37
Acta Geodaetica et Geophysica Hungarica : Volume 36
Acta Geodaetica et Geophysica Hungarica : Volume 35
Acta Geodaetica et Geophysica Hungarica : Volume 34
Acta Geodaetica et Geophysica Hungarica : Volume 33
Acta Geodaetica et Geophysica Hungarica : Volume 32

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Ground motion models — State of the art

Content Provider Springer Nature Link
Author Stamatovska, G. S.
Copyright Year 2008
Abstract Ground motion models represent empirical mathematical-physical models of ground motion under strong earthquakes defined on the basis of databanks of past earthquake records. Within these, the ground motion parameters as dependant random variables are related to the earthquake parameters, the seismic energy transfer characteristics of the region through which the seismic waves propagate and the influence of the local soil conditions as independent random variables. Regression analysis, either single or double, can be applied as a method for their determination. They are used in deterministic and probabilistic methods for prediction and estimation of the expected seismic action of future earthquakes upon the investigated location or region.Ground motion models are very important for prediction of future seismic actions and have been paid special attention. Following the analysis of a variety of published ground motion models for shallow and subduction earthquakes carried out by different authors, there are predictive equations, methods, synthesis, discussions on the state of the art and new trends in investigations of ground motion models.In this study, the author’s attention has been focused on the new ground motion model dependant on the azimuth, which the author has developed and applied for determination of peak ground acceleration attenuation laws for the Vrancea intermediate earthquakes (Stamatovska 1996, 2002, 2006, Stamatovska and Petrovski 1997). Besides the already published results for the peak ground acceleration attenuation laws-PGA for the locations Bucharest, Cherna Voda, and Valeni, the author presents, for the first time, the progress of the applied ground motion model dependent on azimuth in determination of the response spectrum attenuation laws for the Vrancea intermediate earthquakes for Cherna Voda and Bucharest locations.
Starting Page 267
Ending Page 284
Page Count 18
File Format PDF
ISSN 12178977
Journal Acta Geodaetica et Geophysica Hungarica
Volume Number 43
Issue Number 2-3
e-ISSN 15871037
Language English
Publisher Springer Netherlands
Publisher Date 2013-02-27
Publisher Institution Quarterly of the Hungarian Academy of Sciences
Publisher Place Dordrecht
Access Restriction Subscribed
Subject Keyword corrected epicentral distance spectral acceleration seismic focus depth Geophysics/Geodesy ground motion model dependant on the azimuth corrected hypocentral distance
Content Type Text
Resource Type Article
Subject Building and Construction Geology Geophysics
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