1887

Abstract

Direct methods for the numerical calculation of the equation of motion are traditionally based on numerical grids with equidistant spacing. The geological model is represented by the definition of its elastic parameters on the gridpoints. The costs in computation time increase with the number of gridpoints.

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/content/papers/10.3997/2214-4609.201409244
1995-05-29
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409244
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