Skip to Main Content

Abstract

An explanation is given of the use of Pirson’s polar chart in calculating the total-intensity anomaly of a two-dimensional body of arbitrary shape. For magnetization by induction in the earth’s field the anomaly is obtained in one excursion overthe body. Nonparallel magnetizations require two excur-sions. A dike body is used to illustrate the application.

You do not currently have access to this chapter.

Figures & Tables

Contents

GeoRef

References

Related

Citing Books via

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal