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Abstract

Linearized inversion of amplitude versus offset (AVO) from multi-offset data consists of weighted stacking. It yields the elastic parameters as traces in terms of bandlimited relative contrasts. (Smith and Gidlow 1987; Lörtzer and Berkhout 1989). The weighted stacking results are displayed as seismie traces. These traces may be considered as spiky relative contrasts convolved with the seismic wavelet.

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/content/papers/10.3997/2214-4609.201410748
1991-05-28
2024-03-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410748
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