SOME NOTES ON THE UTILIZATION OF A VERTICAL MAGNETIC DIPOLE TO DETERMINE THE PROPERTIES OF A STRATIFIED EARTH.
Abstract
The fields of a vertical magnetic dipole (VMD) located over a stratified earth are derived for the quasi-static range (absolute value gamma sub o rho << 1) and z = h = 0. It is demonstrated that the VMD method may be used in connection with the dipole-dipole method in order to resolve the electrical properties of a simple three-layer model earth (rho sub 1 << rho sub 2 >> rho sub 3). (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Oct 05, 1965
- Accession Number
- AD0622228
Entities
People
- Peter R. Bannister
Organizations
- Navy Underwater Sound Laboratory