Abstract
An overview is given of examples showing the utility of the Comprehensive Model (CM) approach in the processing of near-surface magnetic anomalies. Effectiveness of CM depends on the spatial and temporal matching of the main and external field variations that it attempts to approximate. Hence, data distribution as well as continuity are particularly important.
Original language | English |
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Pages (from-to) | 784-785 |
Number of pages | 2 |
Journal | The Leading Edge |
Volume | 22 |
Issue number | 8 |
DOIs | |
State | Published - Aug 1 2003 |
ASJC Scopus subject areas
- Geophysics
- Geology