1887

Abstract

Amplitude versus offset (avo) interpretations involve a large volume of data. In order to carry out lithologic predictions, the avo data is reduced and simplified by various methods: avo gradients, zero offset amplitudes, even common mid point (cmp) stacks. All these displays are simplifications of a data set that may be influenced by several amplitude factors, such as lithology, tuning effects, correlated noise etc.

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/content/papers/10.3997/2214-4609.201410850
1991-05-28
2020-06-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410850
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