In this work, we are concerned with aspects of seismic data that show frequency dependence. It is at the outset unnecessary to justify this study because those involved in acquisition, processing, and interpretation of seismic data are faced with strong frequency dependence every day. At first impression, the topic seems self-evident: "Of course everything is frequency dependent." However, consider the vast theoretical edifice of acoustic and elastic wave propagation erected since the 1860s. Wave speeds, reflection coefficients (and therefore AVO), geometric decay, Snell's law, and many other topics typically are presented as being independent of frequency.
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