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1.50<br />

1.40<br />

1.30<br />

1.20<br />

1.10<br />

(5% Damping)<br />

Magnitude 9.0 Target Spectrum<br />

Scaled Aeropuerto Ground Motion<br />

Scaled Ofunato Ground Motion<br />

Spectral Acceleration (g)<br />

1.00<br />

0.90<br />

0.80<br />

0.70<br />

0.60<br />

0.50<br />

0.40<br />

0.30<br />

0.20<br />

0.10<br />

0.00<br />

0 0.5 1 1.5 2 2.5<br />

Period (sec)<br />

3<br />

Figure 8.7: Aeropuerto and Ofunato (Scaled PGA = 0.14g) Response Spectra Compared to the Magnitude 9.0<br />

Cascadia Subduction Zone Target Spectrum on Rock<br />

Table 8.4: Attenuation Relationship Input Parameters with the Resulting PGA rock Values<br />

EARTHQUAKE ATTENUATION MAGNITUDE SOURCE-TO-SITE<br />

SOURCE<br />

RELATIONSHIP<br />

DISTANCE (km)<br />

Crustal Abrahamson & Silva (1997) 6.2 8 0.30g<br />

Crustal Boore et al. (1997) 6.2 8 0.20g<br />

Crustal Campbell (1997) 6.2 8 0.36g<br />

Crustal Average 6.2 8 0.29g<br />

Crustal Abrahamson & Silva (1997) 7.0 8 0.45g<br />

Crustal Boore et al. (1997) 7.0 8 0.31g<br />

Crustal Campbell (1997) 7.0 8 0.40g<br />

Crustal Average 7.0 8 0.38g<br />

Subduction Youngs et al. (1997) 8.5 85 0.12g<br />

Subduction Youngs et al. (1997) 9.0 85 0.14g<br />

PGA rock<br />

153

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