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Deep characterization of the Santiago Basin using HVSR and cross-correlation of ambient seismic noise
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文摘

Time- and frequency-domain cross-correlation methods are proposed for basin scale studies.

Rayleigh phase velocity dispersion curves are calculated from 0.1 to 8 Hz.

Seismic ambient noise highly correlates in stations over stiff soil deposits of the Basin.

Shear wave velocity profiles of Santiago gravels have a pronounced increase rate with depth.

The impedance contrast between the Santiago gravels and the underlying bedrock is negligible.

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