1887

Abstract

Geological knowledge will help traveltime inversion to determine the shape of geological structures quantitatively. We consider various least-squares criteria: parallelism, developability and smoothness of folded interfaces, borehole dip measurements, and a new criterion related to the direction of fold axes. Numerical results demonstrate the feasibility of our approach. This work aims at integrating geology and geophysics quantitatively via multicriteria optimization.

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/content/papers/10.3997/2214-4609.201410480
1992-06-01
2020-11-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410480
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