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Site Amplification effects based on Teleseismic Wave ... - METNET

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Mapping of Valley Geometry<br />

<br />

<br />

<br />

<br />

Computati<strong>on</strong> of P-wave arrival time delays and<br />

relative amplitude of the initial P-waves carried<br />

out w.r.t. Pe03 reference stati<strong>on</strong><br />

C<strong>on</strong>sidering P-wave <strong>on</strong>ly in to account, the<br />

unprocessed teleseismic signal is bandpass filtered<br />

between 0.2 – 1.0 Hz, as per S/N ratio in<br />

relatively shorter window length<br />

P-wave time delays are carefully determined by<br />

cross-correlating the first quarter-cycle of the<br />

initial P-waveform of each stati<strong>on</strong> w.r.t. Pe03<br />

reference stati<strong>on</strong><br />

Also the amplitude ratio of the first P-wave<br />

arrivals are determined w.r.t. refrence stati<strong>on</strong>

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