1887

Abstract

Although acoustic wavefield inversion is widely used, a complete solution of the seismic inversion problem requires that we account properly for the physics of wave propagation, and so must include elastic effects. We have developed a 3D tomographic wavefield inversion code that incorporates the full elastic wave equation. The code uses explicit time-stepping by finite differences that are 4th order in space and 2nd order in time.

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/content/papers/10.3997/2214-4609.20149927
2010-06-13
2020-04-07
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20149927
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