Full-3d Seismic Waveform Inversion 2015
DOI: 10.1007/978-3-319-16604-9_6
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CVM-S4.26

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Cited by 8 publications
(4 citation statements)
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References 184 publications
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“… a Values from Willis and Clahan (2006). b Zx indicates the depth to the sediment layer with X km/s shear-wave velocity—values from CVM-S4.26 M01 (Chen and Lee, 2015). …”
Section: Description Of Stochastic Gmm and Physics-based Site Datamentioning
confidence: 99%
See 1 more Smart Citation
“… a Values from Willis and Clahan (2006). b Zx indicates the depth to the sediment layer with X km/s shear-wave velocity—values from CVM-S4.26 M01 (Chen and Lee, 2015). …”
Section: Description Of Stochastic Gmm and Physics-based Site Datamentioning
confidence: 99%
“…Each fault considers multiple hypocenters and slip distributions—hypocenters are placed every 20 km along the strike, and two slip distributions are run for each hypocenter. An anelastic wave propagation simulation calculates strain Green’s tensors (SGTs) using the SCEC Community Velocity Model (CVM) 4.26 (Chen and Lee, 2015) using a parallelized anelastic finite-difference algorithm. Seismic reciprocity is applied to post-process SGT and to obtain synthetic seismograms (Graves and Wald, 2001; Zhao et al, 2006).…”
Section: Description Of Stochastic Gmm and Physics-based Site Datamentioning
confidence: 99%
“…Case study site locations in the Los Angeles basin: (a) topographic map with site locations and fault traces; (b) contour map of Z 2.5 , where Z 2.5 indicates the depth to sediment layer with 2.5 km/s shear-wave velocity, values from velocity model CVM-S4.26 (Chen and Lee 2015). …”
Section: Case Study Sites and Structuresmentioning
confidence: 99%
“…Once the ruptures and their variations are defined, CyberShake uses an anelastic wave propagation simulation to calculate strain Green tensors around the site of interest. The Green tensors are calculated via reciprocity within the prescribed 3D velocity structure (obtained from the SCEC CVM4.26, Chen and Lee, 2015) using a parallelized anelastic finite difference algorithm (Graves, 1996; Graves and Wald, 2001). Seismic reciprocity is used to process the Green tensors and obtain synthetic seismograms (e.g.…”
Section: Introductionmentioning
confidence: 99%