1.17 Kalkan and Gülkan
(2004)
1)
Reference
Erol Kalkan and Polat Gülka, 2004, Empirical
Attenuation Equations for Vertical Ground motion in
2)
Estimated
physical parameter
- Peak ground acceleration (Vertical)
- Pseudo-absolute spectral acceleration (h=5%, T=0.1 to 2.00
sec) (Vertical)
3)
Used strong motion data
- Area:
- Type of earthquake: Shallow crustal
earthquake
- Period: 1976-2002 years
- Number of events: 47
- Number of records: 100
- Magnitude: Mw4.5-7.4
- Epicentral distance:
4)
Style
of faulting
(a)
(b) Strike-slip
(c) Reverse
5)
Ground
condition
(a) Rock (VS=700m/sec)
(b) Soil (VS=400m/sec)
(c) Soft soil (VS=200m/sec)
6)
Definition
of magnitude
Moment magnitude
7)
Definition
of source distance
Closest
horizontal distance
8)
Definition
of horizontal component
Not specified
9)
Applicability
written in the paper
Closest
horizontal distance <200km, Mw 4.5-7.5
10) Empirical attenuation formula
Y: vertical peak ground acceleration or
pseudo-absolute vertical spectral acceleration (g)
M: moment magnitude
rcl:
closest horizontal distance from the station to a site of interest (km)
C6, C7: soil and
soft soil amplification parameter with respect to rock
σ: standard
deviation
P: a value of 0 for mean values and 1
for 84-percentile of lnYV
Table 1.17-1
Coefficients for vertical PGA and 5-percent-damped spectral accelerations