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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.

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View direction is from SW.

 
TMI at different latitudes with varying intensity of the Earth's magnetic field
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Earth's Field
25,000 gamma  35,000 gamma  44,000 gamma  50,000 gamma  56,000 gamma  64,000 gamma  70,000 gamma 
Comment
Notice the orthogonal plug symmetry.            Notice the radial plug symmetry 

Key
Survey Specifications
Scales
plug
k = 10-2
dyke
k = 10-2
background
k = 0
image width
10,000 m
flying height
80 m

3000



-2000

max



min

All models created using
Noddy
Copyright © 1998 AGCRC & Mark Jessell

WWW conversion by Ian Brayshaw