1.5 The effect of changing latitude on anomaly shapes in magnetic data
The sequence of images show the effect on anomaly shape of
calculating the TMI for an East-West dyke and vertical cylinder,
at different southern hemisphere latitudes. For latitudes between
-30°S and -60°S the anomaly shapes are quite similar, with the
main changes being the increasing anomaly amplitude with higher
latitudes (because the Earth's field increases in intensity
towards the poles). At latitudes near the pole and the equator the
anomaly shape starts to become noticeably more symmetric, with
highs over the bodies at the pole and lows over the bodies at the
equator.
The cylindrical plug shows only orthogonal symmetry at the
equator, whereas at the pole it shows radial symmetry.
Note how the offset of the magnetic high varies with latitude.
The grey scale images share a fixed look up table to illustrate
the anomaly amplitude variations. The colour images each have a
look up table clipped to their maximum and minimum values to
highlight the anomally shapes.
The plug is centred at 4800N 4000E and the dyke is centred on
2100N. The grid overlay has 1000 m spacing.
Click on the images to launch Noddy.
A legend is provided at the end of this page.
View of 500 m wide East-West dyke and 1000 m radius vertical cylindrical plug.