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Fig. 9. | Earth, Planets and Space

Fig. 9.

From: Examination of source fault model for the Gifu-Ichinomiya fault based on seismic intensity data

Fig. 9.

Relationship between the predominant periods of the H/V spectral ratio of microtremors and the estimated seismic intensities based on the questionnaire-based intensity of Muramatu and Kominami (1992) and the damage ratios of wooden houses of Muramatu (1983). Diamonds and squares show the points with a seismic intensity of 6 and 7, respectively. Closed symbols also indicate the points that have a predominant period shorter than approximately 0.4 s.

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