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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.


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