Article ID Journal Published Year Pages File Type
4739377 Russian Geology and Geophysics 2010 6 Pages PDF
Abstract

This paper presents a method for restoring missing seismic traces by using the two-dimensional dip moveout (DMO) equation. A fundamentally new formulation of the initial-boundary-value problem based on the Goursat problem is proposed. A modified finite element method is used for numerical solution. The method is tested on model examples and actual seismic data.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology