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- Study of earth's
magnetic field as has existed during geologic time.
Source: Leet, L. Don. 1982.
Physical Geology, 6th Edition. Englewood Cliffs, NJ: Prentice-Hall
- Faint magnetic polarization of rocks that may have been preserved since
the accumulation of sediment or the solidification of magma whose magnetic
particles were oriented with respect to the Earth's magnetic field as it
existed at that time and place. AGI
Source:
Dictionary of Mining, Mineral, and Related Terms
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