The relationships between the various magnetic anomaly components are developed from fundamental theory. A symbolism is introduced which permits expression of the relationships in algebraic form. These techniques have been found useful in predicting anomaly shapes for any magnetic latitude and in simplifying calculations of aeromagnetic or other component intensity anomalies for rock masses. Two examples of the application are shown.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not currently have access to this article.