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Aeromagnetic surveys are used for geophysical prospecting. Some variations in magnetic measurements are caused by rocks that contain significant amounts of magnetic minerals (magnetite being the most common). These anomalies reflect variations in the amount and type of magnetic material and the shape and depth of the body of rock. The features and patterns of aeromagnetic anomalies can also be used to delineate details of subsurface geology including the locations of buried faults and the thickness of surficial sedimentary rocks.
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Are there legal restrictions on access or use of the data?Access_Constraints: none
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Reference herein to any specific commercial product, process, or service by trade name,trademark, manufacturer, or otherwise does not constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof.
Data format: | Flight-line airborne magnetic anomaly measurements, digitized from paper in format CSV (version 1.0) Size: 0.17175483703613 |
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http://mrdata.usgs.gov/geophysics/surveys/geophysics3/ME/me0283.txt |