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Ground motion simulations in the Pollino region (Southern Italy) for Mw 6.4 scenario events. ITIS023 Mercure Basin Fault ITCS038 Remediello-Mormanno Composite source DISS reports that the seismogenic potential associated to such faults is Mw 6.4. Source Model – Mercure Basin Fault.
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Ground motion simulations in the Pollino region (Southern Italy) for Mw 6.4 scenario events
ITIS023 Mercure Basin Fault ITCS038 Remediello-Mormanno Composite source DISS reports that the seismogenic potential associated to such faults is Mw 6.4.
Source Model – Mercure Basin Fault Lenght=22km ; Width=13km Strike, dip, rake= 335° , 60°, -90° Top depth = 1 km Mw=6.4 Slip distribution = Heterogeneous (with 2 main patches of slip) rupture velocity = 0.8 Vs Approximated 1D wave-propagation (ray theory)
Spectral attenuation model R=10km R=50km Rovelli et al., 1988 Cantore et al., 2011 – Irpinia 1<f<30 Hz Castro et al., 2004 – Basilicata 2<f<10 Hz GR=1/R Vs= 3.4 km/s κ =0.035 s
DSM • Syntheticseismograms are computedthrough a modified versione of the stochasticmethodproposedbyBoore(1983) forpoint source model: • Gaussiannoiseismodulatedwithaccelerationenvelopes, computedsolving the rapresentationtheoremforanextend source • The amplitudes are scaledapplying a Reference Fourier spectrum, whoseparameters (corner frequencyand distancefrom the fault ) are inferredfrom the modellingof the extend source. Synthetic Seismogram Random Noise Deterministic Envelope IFFT (point-source-like Reference Spectrum) = X
Ground motionmaps (PGA bedrock) scenario 1: northwestern rupture propagation
Ground motionmaps (PGA bedrock) scenario 2: bilateral rupture propagation
Ground motionmaps (PGA bedrock) scenario 3: southeastern rupture propagation
Ground motionmaps (PGA bedrock) GMPE scenario: ITA10 mean predictions
Acc. Response Spectra at 2 sites Mormanno Lauria
Strong motion data from RAN and INGV stations INGV stations