These models show some of the possible causes of asymmetry in
gravity and magnetic anomalies. The first shows the symmetric
anomaly due to a uniformly magnetised sphere at the South Pole and
the subsequent images show the effect of individually varying the
inclination of the Earth's magnetic field, adding a remanent
magnetisation to the sphere, changing the shape of the body to an
ellipsoid, varying the rock properties within the sphere and
finally measuring the field at a non-uniform height above the body.
The grid spacing is 1000 m and the sphere is centred over
4000E 4000N.
Similar images are also displayed for gravity models.
Geology is viewed from SE.
Click on the images to launch Noddy.
A legend is provided at the end of this page.
This body shows a radially symmetric gravity and an asymmetric magnetic field with an EW symmetry plane. The remanent vector has an inclination of 45° and a declination of 90°.
This body shows asymmetric gravity and magnetic fields with an EW symmetry plane. Panels of equal rock properties dip at 45° towards 90° (red is high density/susceptibility).
Spherical body calculated at South Pole with variable survey heights