| 1. | This is called " detrital remanent magnetization ".
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| 2. | In the later 1AESS, the reeds themselves were of remanent magnetic material.
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| 3. | As mentioned above, magnetofossils hold a remanent magnetization when they are formed.
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| 4. | This phenomenon is called hysteresis and the remaining magnetic field is called remanent magnetism.
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| 5. | The natural remanent magnetization of an igneous rock can be altered by this process.
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| 6. | Minerals that are Ferromagnetic minerals such as magnetite also can carry a remanent magnetization or remanence.
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| 7. | The aplite is the lowest melting remanent of the granite magma, that is poor in volatiles.
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| 8. | The natural remanent magnetization is the permanent magnetism remaining in a rock or sediment after it has formed.
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| 9. | This remanent magnetization, or " remanence ", can be acquired in more than one way.
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| 10. | The sediments also acquire depositional remanent magnetization which allows them to be correlated with earth's geomagnetic reversals.
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