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°N and 60°N 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.