Magsat Session ly, the Great basin of Nevada and southern California, the Rio imposed on a map of Australia. This display is useful for only a Grande rift, and the Mississippi embayment). As mentioned relatively small number of profiles and retains the fidelity of the above, these observations agree quite closely with existing aeromagnetic data along each profile. This display tends to resemble the final broad scale variations in crustal field are caused by magnetic induction. The pixel display is particularly with the Bangui low correspond in both sign and geometry to good at highlighting level errors between adjacent and intersecting anomalies that would be theoretically predicted for the case of profiles.
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