Articles | Volume 11, issue 6
Research article
09 Nov 2020
Research article |  | 09 Nov 2020

Using horizontal-to-vertical spectral ratios to construct shear-wave velocity profiles

Janneke van Ginkel, Elmer Ruigrok, and Rien Herber

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Cited articles

Aki, K. and Richards, P. G.: Quantitative Seismology, University Science Book, Sausalito, California, 704 pp., 2002. a, b
Albarello, D. and Lunedei, E.: Combining horizontal ambient vibration components for H/V spectral ratio estimates, Geophys. J. Int., 194, 936–951, 2013. a, b
Arai, H. and Tokimatsu, K.: S-wave velocity profiling by inversion of microtremor H/V spectrum, B. Seismol. Soc. Am., 94, 53–63, 2004. a, b
Arai, H. and Tokimatsu, K.: S-wave velocity profiling by joint inversion of microtremor dispersion curve and horizontal-to-vertical (H/V) spectrum, B. Seismol. Soc. Am., 95, 1766–1778, 2005. a
Bard, P.-Y.: Microtremor measurements: a tool for site effect estimation, The effects of surface geology on seismic motion, The effects of surface geology on seismic motion, 3, 1251–1279, 1999. a
Short summary
Knowledge of subsurface velocities is key to understand how earthquake waves travel through the Earth. We present a method to construct velocity profiles for the upper sediment layer on top of the Groningen field, the Netherlands. Here, the soft-sediment layer causes resonance of seismic waves, and this resonance is used to compute velocities from. Recordings from large earthquakes and the background noise signals are used to derive reliable velocities for the deep sedimentary layer.