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natural remanent magnetization |
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natural remanent magnetization [′nach·rəl ′rem·ə·nənt ‚mag·nə·tə′zā·shən]
(geophysics) The magnetization of rock which exists in the absence of a magnetic field and has been acquired from the influence of the earth's magnetic field at the time of their formation or, in certain cases, at later times. Abbreviated NRM. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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