1887

Abstract

Geophysical data is frequently collected in vast quantities, resulting in large amounts of data that<br>oten require rapid interpretation. Semi-automatic interpretation methods, such as Euler (Hood 1963, Reid<br>et al 1990, Durrheim and Cooper 1998, Barbosa, Silva, and Medeiros 1999) and Werner (Hartman, Teskey,<br>and Friedberg, 1971) deconvolution can assist the interpreter by indicating portions of the data of interest,<br>which can then be modeled in detail.

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/content/papers/10.3997/2214-4609-pdb.143.10.1
2001-10-09
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.143.10.1
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