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Abstract

To evaluate the results of AVO-inversion procedures, the offset-depending amplitudes are extracted from a P- respectively PS-wave section after very careful data processing. To these, the calculated reflection coefficients of likely lithology models are fitted.

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/content/papers/10.3997/2214-4609.201411594
1993-06-08
2025-02-13
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/content/papers/10.3997/2214-4609.201411594
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