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INTEGRATED GEOLOGICAL-GEOPHYSICAL INTERPRETATIONS


THE ROLE OF AEROMAGNETIC DATA IN EXPLORATION

Aeromagnetic data reflect the varying rock types in the crust. Quantitative interpretations of aeromagnetic data, integrated with the known surface geology, can delineate many structures and plutons that control the location of mineralization. Major, deep-seated structures are often manifested in the magnetic data by alignments of magnetic discontinuities. Plutons, particularly those of Tertiary age, frequently exhibit prominent magnetic anomalies. As a general principal, low-level surveys are more influenced by variations in near-surface rocks, and higher level surveys "look" deeper, i.e. they map changes in rock-types at greater depth.


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