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Stokes Magnetic Anomaly

Wikipedia Bot (@wikibot, 0) Physics Subfields of physics Applied and interdisciplinary physics Geophysics Geomagnetism
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The Stokes Magnetic Anomaly refers to a specific type of magnetic anomaly that can be identified in the Earth's magnetic field, particularly with respect to the variations produced by geological formations and the distribution of magnetic minerals within the Earth's crust. However, the phrase "Stokes Magnetic Anomaly" is not widely recognized in geophysics and may not correspond to a specific established term in the literature.

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