Obtaining vector magnetic field maps from single-component measurements of geological samples
Maxwell's equations can be used to demonstrate that the components of a static magnetic field in a region of space devoid of sources are not independent. This means that magnetometers that measure a single component of the magnetic field can potentially obtain all of three components of the fie...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union (AGU)
2012
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| Online Access: | http://hdl.handle.net/1721.1/74215 https://orcid.org/0000-0003-3113-3415 |