S-wave velocity images of the Dead Sea Basin provided by ambient seismic noise
Journal of Asian Earth Sciences(2013)
Abstract
•We have applied passive seismic interferometry to ambient seismic noise.•The explored frequency range was the secondary microseism bandwidth 0.1–0.5Hz.•We display S-wave velocity sections of the Dead Sea Basin at depths 0–11km.•The bowl-shaped basin, its asymmetrical structure and infill materials are shown.
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Key words
Ambient seismic noise,Correlation,Dispersion,Tomography,Depth-dependent shear velocity models,Dead Sea
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