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Preliminary PEER-NGA Ground Motion Model
Brian Chiou and Robert Youngs PEER-NGA Workshop April 12, 2005
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Data Selection Excluded earthquakes Excluded records
Gorda plate earthquakes – oceanic crust Subduction zone earthquakes Poorly known overseas earthquakes Northwest China earthquakes Earthquakes recorded by SMART1 array Aftershocks (used only in site effects analysis) Excluded records In basements In large structures On dam abutment
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Modeling Concepts Source scaling Distance scaling Magnitude (M, M2.5 )
No aspect ratio Depth (depth to the top of rupture) Style of faulting (SS+NM vs. RV) Aftershocks not used Distance scaling Closest distance to fault Effect of Q for large distances Break in slope at about 60 km Hanging wall effects, function of fault dip angle
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Modeling Concepts (cont’d)
Site Effects Function of VS30 (will examine effect using categories) Nonlinear site amplification (using empirical data guided by modeling results) Depth to VS ~ 1 km/s
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Model Form Reference site motion (Vs=1130m/sec) Site effects yr ys
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a ln(yr) c b Amplification relative to Vs=1130 m/sec
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PGA Comparison to Site Response Analysis with EPRI Soil Property Model
Analysis (EPRI Soil) Regression
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Comparison to Site Response Analysis with Peninsula Range Soil Property Model
PGA Site Response Analysis (Peninsula Rage Soil)
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Comparison to Site Response Analysis with EPRI Soil Property Model
T=1 Sec Site Response Analysis (EPRI) Regression
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Comparison to Site Response Analysis with Peninsula Range Soil Property Model
PGA
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Soft Rock, Strike Slip and Reverse PGA
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Strike Slip Soft Rock and Soil PGA
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Strike Slip Soil PGA and 1 Hz PSA
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Inter-event Residuals
Magnitude Distance
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PGA Intra-event Residuals
Magnitude Distance
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1 Hz PSA Intra-event Residuals
Magnitude Distance
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T=3Sec
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T=3Sec
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Dip Slip Earthquakes, Records on HW/FW
T=3Sec
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T=3Sec
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