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Why are we interested in potential field data as an aid to geological mapping? There are generally insufficient geological observations to unambiguously construct the boundaries between formations to form a 3D geological map. Observations are generally in short supply at depth and relationships between formations may be unclear. Variations in potential field response are related to the 3D distribution of physical properties. If we can sensibly relate physical properties to the units used in the geolog

Author

Fan3093

Language

EN