Statistical determination of the depth of occurrence of sources of magnetic field anomalies
Authors:
Abstract
One of the tasks often solved using aeromagnetic survey data is to determine the depth of occurrence of magnetized rocks. The experience of using AT anomalies in different geological regions shows that the results of calculations become quite reliable only after statistical generalization. In the simplest case, the values of the depth of occurrence of disturbing masses are averaged over some area, for example, within a single anomalous zone, or over part of the route.
Область исследования:
(Archived) Geology and geophsics
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