1887

Abstract

Amplitude scattering, caused by the occurence of thin gaps between layers, is a fractal phenomenon that may generate visible events on seismic sections, correlated from trace to trace but different from usual reflections, although of equivalent energy.

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/content/papers/10.3997/2214-4609.201406735
2001-04-30
2024-10-09
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/content/papers/10.3997/2214-4609.201406735
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