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Fig. 4 | Earth, Planets and Space

Fig. 4

From: Estimation of shallow S-wave velocity structure and site response characteristics by microtremor array measurements in Tekirdag region, NW Turkey

Fig. 4

Observed Rayleigh wave phase velocities dispersion curves of 42 sites in Tekirdag obtained by the SPAC method. The sites are grouped according to their geological units: a alluvial, b resent landfill, c claystone, d sandstone, e siltstone, f clay-sand stone, continental clastic rocks, carbonates, Muratli, Corlu (g), and Marmara Ereglisi (h)

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